Plio-Pleistocene Behavior of the Itoigawa-Shizuoka Tectonic Line in Northern Nagano Prefecture, Central Japan: Paleomagnetism of the Omine-SK++*
|
|
- Σίβύλλα Σκλαβούνος
- 5 χρόνια πριν
- Προβολές:
Transcript
1 Bull Earthq Res Inst Univ Tokyo Vol 2-,**2 pp : SK++* + * + Plio-Pleistocene Behavior of the Itoigawa-Shizuoka Tectonic Line in Northern Nagano Prefecture, Central Japan: Paleomagnetism of the Omine-SK++* Tephra + Takeyuki Ueki * + Institute of Geology and Geoinformation, Geological Survey of Japan, AIST Abstract This study aims to reveal Late Pliocene to Early Pleistocene geomorphic and structural evolution of the Omine Belt, North Fossa Magna, central Japan, associated with tectonic movement of the Itoigawa-Shizuoka tectonic line A comparison of the paleomagnetic directions of a distinct wide-spread tephra, which is exposed in di# erent areas, is useful to detect tectonic rotation because it gives instantaneous paleomagnetic directions from proximal to distal areas The Omine-SK++* tephra with an estimated age of + 0/ + 0* Ma is distributed in the Omine Belt as Omine Welded Tu# and in the west Tama Hills of the Kanto Plain as a co-ignimbrite of the Horinouchi, Tu # Progressive alternating field and thermal demagnetization experiments reveal that both tephras have reversed paleomagnetic directions that are almost identical to each other As the west Tama Hills had been in a tectonically stable area since Late Pliocene, there might be no vertical-axis rotation in the Omine Belt Thus, the Omine Belt would not be a pull-apart basin with left-lateral strike-slip faulting between the Otari-Nakayama fault and the active fault system of the Itoigawa-Shizuoka tectonic line Key words: Itoigawa-Shizuoka tectonic line, Omine-SK+** tephra, paleomagnetism, Early Pleistocene, thrust front migration + +32/ ; +321 ; +33* ; +33+ ; +331 ; +332 ;,**+,**0; Okumura,,**+;,**0 / m+*** +/* km,**+; Matsuta et al, + : +33+ ; ;,** +3 ; Okumura,,**+ -* km * km Elouai et al,,**; Sato et al, + 0 m+*** Une,** ab * gakusetsu-ueki@aistgojp -*/ 2/
2 ; ; Takeuchi,,** Elouai et al,,**; Sato et al,,** ab Ikami et al, +320 ; +321; Fig + Index map of the Itoigawa-Shizuoka tectonic,***;,**+,**1ab; Elouai et line (ISTL), Omine Belt in the north Nagano Prefecture and Tama Hills in the western flank of al,,**; Sato et al,,** ab;,**/ Kanto Plain, central Japan Shaded area indicates the North Fossa Magna Bold line on the ISTL indicates the active fault system AMR, OKH and PHS are the Amurian, Okhotsk and Philippine Sea Plates +333 SK++*,*** SK++*,** / +* km ;,***;,**-, +32* , +32- ; +323 ; , 0 -, / thrust front migration: Ikeda, +32-,,**,; Ueki,,**, 0/ km, / +* km,,**, +33+,* * 164
3 SK++* Fig, Geology of the central to south Omine Belt and surrounding areas, and sampling sites for the Omine Welded Tu# Geologic map is simplified after and Yamada et al ( +323 ) and Kosaka ( +33+ ) + 0 are the sampling sites for the Omine Welded Tu # EMF, KF, ONF and TF are the Eastern Margin fault of the Matsumoto Basin, Kamishiro fault, Otari-Nakayama fault and Terama fault +/ ; +2 ; +32- ; ; +323 ; / Ma,*** ** m +331 SK++*,***,**-,*** SK++* SK++* +0/ +0 Ma +331 ;,***;,** Ma K-Ar FT,,**/ +3-- ; ; , +33 Kd,/ +3,*** Kd,/,,**,,**,, SK++* 0,, /
4 Fig - Geology of the west Tama Hills and sampling sites for the Horinouchi, Tu# Geologic map is simplified after Takano ( +33 ) 1 ++ are the sampling sites for the Horinouchi, Tu # Fig Geologic columnar sections of the Oyamada Formation of the Kazusa Group intercalated with cm 1 the Horinouchi, Tu # (HU,) Location of the Site 1++ are shown in Fig - ++, / +* cm +*,* cm,* mm, -, progressive alternating field demagnetization, PAFD progressive thermal demagnetization, PThD 3, - 0 PAFD PThD -,/ cm + + PAFD,/ cm 1 2 +* ++, 1 / 2, + PThD 3,/ cm 1, PAFD PThD +,, 166
5 SK++* PAFD PThD nent magnetization, VRM PAFD, G /,* mt 2* mt 2* mt, / 10* R PAFD * +* mt VRM,/ mt +* 2* mt / mt ++, /* PThD Magnetic Measurements MMTD-+2 PThD 0/*, MAD *-,, + 0,* +** /** /* PThD +/* /** 0/* -* * + VRM / + A -* PAFD, PThD, 0 Zijderveld, ** Kirschvink, +32* VRM 0 B, + / maximum angular deviation, +/*,** /3* MAD +/ / + A, 0 3, PAFD PThD ** ** PAFD /0* / 0 A 3,, 0,* VRM PThD +* + PAFD PAFD, PThD MAD * /3 0,+ - /0 3 McFadden and MacElhinny * 3,** PThD PAFD 0* PThD 3 a : Fisher, +- k: Fisher, +- +, /,* - -*-* ,, 2, -*, +++ / +,,, PAFD 1 2 +* ++ : 1 2 +* ++ PAFD, PThD PAFD /,/ mt PThD / ,/ +*,133 + / 1 A+ VRM PAFD -2mT * 1 --/ mt /* 2* mt / + A 2* mt + 0 B+ Brunhes 1 VRM Chron Viscous rema /
6 Fig / Progressive alternating field and thermal demagnetization (PAFD and PThD) results for representative samples of the Omine-SK+** tephra plotted on orthogonal vector diagrams Solid and open circles are the projections in the geographic coordinates of remanence vectors on the horizontal, and north-south vertical planes, respectively Unit of magnetization intensity is Am 168
7 SK++* Fig 0 Equal-area projections of site-mean remanent magnetization directions of the Omine-SK +** tephra + Site-mean (open circles) and overall mean (open rectangles) remanent magnetization directions of the Omine Welded Tu # Remanent magnetization directions are projected in the upper hemisphere Gray ovals correspond to the confidence cones of the overall mean remanent magnetization direction mdec and minc are overall mean declination and inclination a, k, N are radius of confidence cone ( ), Fisher s ( +-) precision parameter, number of sampling sites +0 are the sampling sites for the Omine Welded Tu #, Site-mean (open circles) and overall mean (open rectangles) remanent magnetization directions of the Horinouchi, Tu # 1, 2, +*, ++ are the sampling sites for the Horinouchi, Tu # - Site-mean remanent magnetization direction (open rectangle) at Loc 3, determined by combination of stable remanent directions and best-fit demagnetization circles following the method of McFadden McElhinny ( +322) mdec and minc are declination and inclination of site-mean remanent magnetization direction Nd and Nc are numbers of stable remanent directions and best-fit demagnetization circles A+ -J+ and A, -J, are the specimens for PAFD and PThD Four open circles are the stable remanent magnetization directions of specimens projected in the upper hemisphere Dashed and solid lines are parts of best-fit demagnetization circles projected in the lower and upper hemispheres, applied for principal component analyses by progressive demagnetization experiments The arrows indicate trend of remanent magnetization direction during progressive demagnetization experiments Gray oval corresponds to the confidence cone of the site-mean remanent magnetization direction +*,33, / 1 A, 1 2 +* ++ +/* ** /0* MAD * ,* +** +/* PThD +** -/* 0,* -** /-* /0* 002 VRM /3* -/* 169
8 Table + Site-mean paleomagnetic data for the Omine Welded Tu# and the Horinouchi, Tu # Omine WT and HU, are the Omine Welded Tu# and Horinouchi, Tu # Latitude and longitude of each locality are shown as the World Geodetic System +32 S and D are strike and dip of sedimentary rocks immediately beneath the Omine Welded Tu # Nd and Nc are the numbers of stable remanent magnetization components and best-fit great circles to calculate the site-mean remanent magnetization directions D and I are declination and inclination of in situ site-mean remanent magnetization directions Dc and Ic are declination and inclination of tilt-corrected site-mean remanent magnetization directions MAD is averaged maximum angular deviation of stable magnetization components a and k are radius of confidence cone ( ) and Fisher s ( +-) precision parameter l and f are latitude and longitude of virtual geomagnetic pole -** /-* 0,* VRM VRM / 3 0,, +* ++ B,,** -** /+ 1 + /3* 0,* 0,* VRM MAD,2 0,3 + +* + + /3* 0,* +** 1 2 +* ++ +0,* , a k / , +1/ * + MAD +* 0 + * + 3 : 3 PThD +* +/*,/* PAFD PAFD +/*,/*,** ** / 3 B+ +/ 0- / mt 2* mt 3 VRM 0,* 2 // VRM 2* 3 VRM mt VRM PThD 3 PThD +** +/* PAFD PThD +** +/*,** -**
9 SK++* + 0- a k 01 -*/ + / / +, + 0, /,,, 1 ++, +1- / /3 * a k 3 + 1, + 0,, / /*/ ,**, * // + /0 *, km 2* a, +323, SK++* thermoremanent 0 magnetization, TRM, detrital remanent magnetization, DRM a k 3 3 1, 0 +, SK++*,,, DRM depositional, detrital remanent magnetization, ddrm,,**,, thrust front migration,**,; Ueki,,**, /,,**, ; ; Takeuchi,,**,: ,*** m
10 Takeuchi,** / / / Kirschvink, JL, +32*, The least-squares line and plane and the analysis of palaeomagnetic data Geophys Jour Roy astron Soc, 0,, / 0+ -* 1,**0 A ++/,*2,,* +32* +/ ,0 1/ +* +333,+ /23 / no , +331 : +*0 -, -3 2,**- --0,**+ Elouai, D, Sato, H, Hirata, N, Kawasaki, S, Takeshita, T,,* /31* Kato, N and Takeda, T,,**, Deep seismic reflection Matsuta, N, Ikeda, Y and Sato, H,,**, The slip rate along profiling across the Northern Fossa Magna : The ERI the northern Itoigawa-Shizuoka tectonic line active +331 and the JNOC +330 seismic lines, active faults and fault system, central Japan Earth Planets Space, /0, geological structures Earth Planets Space, /0, ,- +--* Fisher, R, +-, Dispersion on a sphereproc Roy Soc London, Ser A,,+1,, -*/ +2,** ,0 +*/ +,* Ikami, A, Yoshii, T, Kubota, S, Sasaki, Y, Hasemi, A, Moriya, T, Miyamachi, H, Matsu ura, RS and Wada, K, +320, A seismic-refraction profile in and around Nagano Prefecture, central Japan Jour Phys Earth, -, /1 1 Ikeda, Y, +32-, Thrust front migration and its mechanism:,**1a evolution of intraplate thrust systems Bull Dep Geogr Univ Tokyo, +/, +,/ +/3 2,,/ -/,**,,0*,**1b 172
11 SK++* 2, -1,0 +,+ +-0 McFadden, PL and McElhinny, MW, +322, The combined +321 analysis of remagnetization circles and direct observa- no +1 3, 3- tions in paleomagnetism Earth Planet Sci Lett, 21, , +3,**, K-Ar,**/ /- -3,/ * ** * ** 01/ 03+,**, +* 2-32 no -, ++ ++/ * ** /* // , /*,3,,+ /2- /22,*** Takeuchi, A,,**, Basement-involved tectonics in North Fossa Magna, central Japan: The significance of the +*0 /+ 03 northern Itoigawa-Shizuoka Tectonic Line Earth Planets +33* Space, /0, +,0+ +,03 2 +/, ,*** A ,**, Okumura, K,,**+, Paleoseismology of the Itoigawa- Shizuoka tectonic line in central Japan Jour Seismol, /, / * 1332*+ Ueki, T,,**,, History of fault activity based on the paleo- 0,/ -2 geography and paleo-geologic-structure since Pliocene: Examples of the northeastern Shikoku Island, southwest +332 Japan, and the Omine area of the Northern Fossa Magna region, central Japan PhD thesis of Tokyo Met- /* -/ /+ ropolitan University, ++0p Sato, H, Iwasaki, T, Kawasaki, S, Ikeda, Y, Matsuta, N,,**/, Takeda, T, Hirata N and Kawanaka, T,,** a, Formation and shortening deformation of a back-arc rift basin ++ 0,-0,/ revealed by deep seismic profiling, central Japan Tectonophysics, Une, H, +32/, On the tectonic landforms in the northwestern -22, 1 /2 part of the Nagano Prefecture, central Japan Bull Sato, H, Iwasaki, T, Ikeda, Y, Takeda, T, Matsuta, N, Imai, Geogr Surv Inst,,3, 22 +*+ T, Kurashimo, E, Hirata, N, Sakai, S, Elouai, D, Kawanaka, +323 T, Kawasaki, S, Abe, S, Kozawa, T, Ikawa, T,,* + Arai, Y and Kato, N,,** b, Seismological and geologi cal characterization of the crust in the southern part of * 2331 northern Fossa Magna, central Japan Earth Planets Zijderveld, JDA, +301, AC demagnetization of rocks : Space, /0, +,/- +,/3 Analysis of results,in Methods in Palaeomagnetism edited +333 by Collinson, D, Creer, K and Runcorn, S, Elsevier, /-,1/,3* pp,/0,20 Received May +/,,**2 Accepted September,3,,**2,**0 173
High-resolution seismic reflection survey across the Western Boundary Fault Zone of the Nagano Basin, Central Japan: Data acquisition and processing
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2+,**0 pp. +1++2* : + * +, -. / 0 1 1 2 3 +, : -. / 0 1 2 : 3 +* : +* High-resolution seismic reflection survey across the Western Boundary Fault Zone of the Nagano
Διαβάστε περισσότεραResurvey of Possible Seismic Fissures in the Old-Edo River in Tokyo
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2.,**3 pp.,,3,.* * +, -. +, -. Resurvey of Possible Seismic Fissures in the Old-Edo River in Tokyo Kunihiko Shimazaki *, Tsuyoshi Haraguchi, Takeo Ishibe +, -.
Διαβάστε περισσότεραHigh-density Seismic Array Observations Across the Northern Focal Area of the,**2 Iwate-Miyagi Nairiku Earthquake
Bull Earthq Res Inst Univ Tokyo Vol 20,*++ pp + +*,**2 + +, + + + + * - - + - - - - +, -, + + + + High-density Seismic Array Observations Across the Northern Focal Area of the,**2 Iwate-Miyagi Nairiku
Διαβάστε περισσότεραDense Seismic Array Observations Along the Hanno- Misaka Line, Kanto Mountains, Central Japan
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2.,**3 pp.,+1,,1 * +, + +, + Dense Seismic Array Observations Along the Hanno- Misaka Line, Kanto Mountains, Central Japan Eiji Kurashimo *, Hiroshi Sato, Susumu
Διαβάστε περισσότεραEmplacement Temperature of the Lithic-rich Pyroclastic Flow of Mt. Vesuvius.1, AD Eruption: Paleomagnetic Measurement
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2,,**1 pp. +13 +3-.1, * +,,, +, Emplacement Temperature of the Lithic-rich Pyroclastic Flow of Mt. Vesuvius.1, AD Eruption: Paleomagnetic Measurement Keiko Suzuki-Kamata
Διαβάστε περισσότεραFocal Mechanism Solutions of Micro- and Small Earthquakes Occurred in the Western Kanagawa Area Situated in the Izu Collision Zone
Bull Earthq Res Inst Univ Tokyo Vol 2,**3 pp,33-*/ * +, + + + + +, + + Focal Mechanism Solutions of Micro- and Small Earthquakes Occurred in the Western Kanagawa Area Situated in the Izu Collision Zone
Διαβάστε περισσότεραMeasuring Crustal Movements with GPS and Temperature of Fumaroles with Radiation Thermometer at Volcano Yake-Dake, Hida Mountains, Central Japan
Bull Earthq Res Inst Univ Tokyo Vol 2/,*+* pp +/ -+ GPS +33,,**2 * Measuring Crustal Movements with GPS and Temperature of Fumaroles with Radiation Thermometer at Volcano Yake-Dake, Hida Mountains, Central
Διαβάστε περισσότεραShallow seismic reflection profiling across the western marginal faults of Kitakami Lowland, northern Honshu Island, Japan
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2+,**0 pp. +-3 +.1 + * +,, - +. / 0 1 +, -. : / 0 1 Shallow seismic reflection profiling across the western marginal faults of Kitakami Lowland, northern Honshu
Διαβάστε περισσότεραDeep Seismic Refraction/Wide-angle Reflection Profiling in Central Japan
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2-,**2 pp. 11 +*+ Deep Seismic Refraction/Wide-angle Reflection Profiling in Central Japan The Research Group for Seismic Expedition in Central Japan Abstract
Διαβάστε περισσότεραRecent Crustal Movement Inferred from GPS Observation of Mt. Tateyama, Northern Alps, Central Japan
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2-,**2 pp. +3-,*+ GPS * +, - +, + + - GPS : Recent Crustal Movement Inferred from GPS Observation of Mt. Tateyama, Northern Alps, Central Japan Ryosuke Doke *,
Διαβάστε περισσότεραSeismic Expedition in the Hinagu Fault Area, Kyushu Island, Japan
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2-,**2 pp. +*- +-* Seismic Expedition in the Hinagu Fault Area, Kyushu Island, Japan +,**0 +333 +333 Kodaira et al.,,**,;,**,; Kurashimo et al.,,**-; Sato et kmo
Διαβάστε περισσότεραSeismic Reflection Profiling Across the North of the Itoigawa-Shizuoka Tectonic Line in Omachi, Central Japan
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2,,**1 pp. -1.. +, -. / - 0-1 2 3 +* ++ +,, +- + :, -. : / : 0 : 1 2 : 3 +* ++ : +, : +- Seismic Reflection Profiling Across the North of the Itoigawa-Shizuoka
Διαβάστε περισσότεραSeismic Reflection Profiling Across the Onshore Source Area of the,**1 Noto Hanto Earthquake, Central Japan
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2,,**1 pp.,0/,1-,**1 * +,, + + - +, - Seismic Reflection Profiling Across the Onshore Source Area of the,**1 Noto Hanto Earthquake, Central Japan +,, + + Hiroshi
Διαβάστε περισσότεραMasaaki Hamada *, Takeo Noguchi, Fumihiro Anada, Koji Nohara, Takahiro Miya- uchi, Kazuki Watanabe, Hiroyuki Yamaguchi
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2,,**1 pp. -./ -/3,**1 + + + +,, - *. +, -. Crustal Deformation Associated with the,**1 Noto Hanto Earthquake and Late Quaternary Marine Terrace Distribution on
Διαβάστε περισσότεραShallow Subseafloor Structure in the Inshore Area o# the Southwestern Part of the Boso Peninsula Imaged by Marine Seismic Reflection Profiling
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2.,**3 pp. -*1-,3 + +,, + + - * +, -... Shallow Subseafloor Structure in the Inshore Area o# the Southwestern Part of the Boso Peninsula Imaged by Marine Seismic
Διαβάστε περισσότερα1, +,*+* + +-,, -*, * : Key words: global warming, snowfall, snowmelt, snow water equivalent. Ohmura,,**0,**
1, +,*+* + +-,, + : /+* m,1+ m, -*, * +3132* : Key words: global warming, snowfall, snowmelt, snow water equivalent + IPCC,,**+ Inoue and,**2 Yokoyama,**- Ohmura,,**0,**0 +331 +332 + +2- **+, ++,* 14 1,
Διαβάστε περισσότερα; +302 ; +313; +320,.
1.,,*+, - +./ +/2 +, -. ; +, - +* cm : Key words: snow-water content, surface soil, snow type, water permeability, water retention +,**. +,,**/.. +30- +302 ; +302 ; +313; +320,. + *+, *2// + -.*, **. **+.,
Διαβάστε περισσότεραHigh-resolution seismic reflection profiling across the Senya fault at Hanaoka, northern Honshu, Japan: Data acquisition and processing
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2+,**0 pp. 31 +*0 : + *, -. / 0 1 1 2 2 3 +* + + + ++ +, +- +. 30 +, - :. : / 0 1 2 3 +* ++ : +, : +- : +. High-resolution seismic reflection profiling across
Διαβάστε περισσότεραHigh-Resolution Seismic Reflection Survey Oguro River Seismic Line in the Ina Valley Fault Zone, Central Japan: Data Acquisition and Processing
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2,,**1 pp. +-,- : + +, -. / 0 1 2 2 3 +* ++ +, +- +. +/ +0 +, : - :. / : 0 : 1 2 3 : +* ++ +, : +- : +. : +/ : +0 : High-Resolution Seismic Reflection Survey Oguro
Διαβάστε περισσότερα* ** *** *** Jun S HIMADA*, Kyoko O HSUMI**, Kazuhiko O HBA*** and Atsushi M ARUYAMA***
J. Jpn. Soc. Soil Phys. No. +*2, p. +3,2,**2 * ** *** *** Influence Area of Stem Flow on a Soil of Deciduous Forest Floor by Electric Resistivity Survey and the Evaluation of Groundwater Recharge through
Διαβάστε περισσότεραDistribution of the Metropolitan Seismic Observation network
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2.,**3 pp. /103 * Distribution of the Metropolitan Seismic Observation network Shin ichi Sakai* and Naoshi Hirata Earthquake Research Institute, the University
Διαβάστε περισσότεραHydrologic Process in Wetland
J. Jpn. Soc. Soil Phys. No. +*-, p.1+12,**0 * Hydrologic Process in Wetland Characteristics of a Mire in a Snowy Region Makoto NAKATSUGAWA** ** Toyohashi O$ce of River Works, Chubu Regional Development
Διαβάστε περισσότεραDevelopment of a Tiltmeter with a XY Magnetic Detector (Part +)
No. 2 +0,/,**, Technical Research Report, Earthquake Research Institute, University of Tokyo, No. 2, pp.+0,/,,**,. XY * * ** *** **** ***** Development of a Tiltmeter with a XY Magnetic Detector (Part
Διαβάστε περισσότερα, Geology, geologic structure, and hot springs in southern Kyushu, Japan
/1,**1 11, Geology, geologic structure, and hot springs in southern Kyushu, Japan +, +3 0 +- +3 0 +. + 23***0/ +,+-/, 23*2/00 +*+ Tetsuo KOBAYASHI + and Toru YANO, + Earth and environmental Sciences, Faculty
Διαβάστε περισσότεραReminders: linear functions
Reminders: linear functions Let U and V be vector spaces over the same field F. Definition A function f : U V is linear if for every u 1, u 2 U, f (u 1 + u 2 ) = f (u 1 ) + f (u 2 ), and for every u U
Διαβάστε περισσότεραb. Use the parametrization from (a) to compute the area of S a as S a ds. Be sure to substitute for ds!
MTH U341 urface Integrals, tokes theorem, the divergence theorem To be turned in Wed., Dec. 1. 1. Let be the sphere of radius a, x 2 + y 2 + z 2 a 2. a. Use spherical coordinates (with ρ a) to parametrize.
Διαβάστε περισσότεραRetrieval of Seismic Data Recorded on Open-reel-type Magnetic Tapes (MT) by Using Existing Devices
No. 3 + 1,**- Technical Research Report, Earthquake Research Institute, University of Tokyo, No. 3, pp. + 1,,**-. MT * ** *** Retrieval of Seismic Data Recorded on Open-reel-type Magnetic Tapes (MT) by
Διαβάστε περισσότεραMSM Men who have Sex with Men HIV -
,**, The Japanese Society for AIDS Research The Journal of AIDS Research HIV,0 + + + + +,,, +, : HIV : +322,*** HIV,0,, :., n,0,,. + 2 2, CD. +3-ml n,, AIDS 3 ARC 3 +* 1. A, MSM Men who have Sex with Men
Διαβάστε περισσότεραΖΩΝΟΠΟΙΗΣΗ ΤΗΣ ΚΑΤΟΛΙΣΘΗΤΙΚΗΣ ΕΠΙΚΙΝΔΥΝΟΤΗΤΑΣ ΣΤΟ ΟΡΟΣ ΠΗΛΙΟ ΜΕ ΤΗ ΣΥΜΒΟΛΗ ΔΕΔΟΜΕΝΩΝ ΣΥΜΒΟΛΟΜΕΤΡΙΑΣ ΜΟΝΙΜΩΝ ΣΚΕΔΑΣΤΩΝ
EΘΝΙΚΟ ΜΕΤΣΟΒΙΟ ΠΟΛΥΤΕΧΕΙΟ Τμήμα Μηχανικών Μεταλλείων-Μεταλλουργών ΖΩΝΟΠΟΙΗΣΗ ΤΗΣ ΚΑΤΟΛΙΣΘΗΤΙΚΗΣ ΕΠΙΚΙΝΔΥΝΟΤΗΤΑΣ ΜΕ ΤΗ ΣΥΜΒΟΛΗ ΔΕΔΟΜΕΝΩΝ ΣΥΜΒΟΛΟΜΕΤΡΙΑΣ ΜΟΝΙΜΩΝ ΣΚΕΔΑΣΤΩΝ ΔΙΠΛΩΜΑΤΙΚΗ ΕΡΓΑΣΙΑ Κιτσάκη Μαρίνα
Διαβάστε περισσότεραApproximation of distance between locations on earth given by latitude and longitude
Approximation of distance between locations on earth given by latitude and longitude Jan Behrens 2012-12-31 In this paper we shall provide a method to approximate distances between two points on earth
Διαβάστε περισσότεραIsotopic and Geochemical Study of Travertine and Hot Springs Occurring Along the Yumoto Fault at North Coast of the Oga Peninsula, Akita Prefecture
J. Hot Spring Sci. /2 **2 * + + + + + +3 ++ * * + 3 Isotopic and Geochemical Study of Travertine and Hot Springs Occurring Along the Yumoto Fault at North Coast of the Oga Peninsula Akita Prefecture +
Διαβάστε περισσότεραEstimation of the Azimuth of MeSO-net Borehole Seismometers Based on Long-period Seismic Ground Motion
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2.,**3 pp. ++/ +,/ MeSO-net +, - - + - + * -. +, -. Estimation of the Azimuth of MeSO-net Borehole Seismometers Based on Long-period Seismic Ground Motion +, -
Διαβάστε περισσότερα* *, ** Koji Masuda* and Takashi Arai*, **
.2,/-*,**. Japanese Journal of Structural Geology, No..2,,/-*,,**. Experimental studies of fracture and friction with gas-medium high-pressure and high-temperature apparatus **, ** Koji Masuda* and Takashi
Διαβάστε περισσότεραReaction of a Platinum Electrode for the Measurement of Redox Potential of Paddy Soil
J. Jpn. Soc. Soil Phys. No. +*0, p.- +*,**1 Eh * ** Reaction of a Platinum Electrode for the Measurement of Redox Potential of Paddy Soil Daisuke MURAKAMI* and Tatsuaki KASUBUCHI** * The United Graduate
Διαβάστε περισσότεραK-Ar. K-Ar Dating of Kimpo Volcano, Northern Ryukyu Arc
/+ (,**0) + -+.* K-Ar,**/ 0,1,**0 + +* K-Ar Dating of Kimpo Volcano, Northern Ryukyu Arc Kiyoshi TOSHIDA, Kozo UTO and Akikazu MATSUMOTO Kimpo volcano is a distinct volcano in central Kyushu, western Japan,
Διαβάστε περισσότεραFrequent and Intensive Eruptions in the 3th Century, Izu Islands, Japan: Revision of Volcano-Stratigraphy Based on Tephras and Historical Document
/+ (,**0) / -,1 --2 3,,**0 / 3,**0 2,3 Frequent and Intensive Eruptions in the 3th Century, Izu Islands, Japan: Revision of Volcano-Stratigraphy Based on Tephras and Historical Document Masashi TSUKUI,
Διαβάστε περισσότεραΚΥΠΡΙΑΚΗ ΕΤΑΙΡΕΙΑ ΠΛΗΡΟΦΟΡΙΚΗΣ CYPRUS COMPUTER SOCIETY ΠΑΓΚΥΠΡΙΟΣ ΜΑΘΗΤΙΚΟΣ ΔΙΑΓΩΝΙΣΜΟΣ ΠΛΗΡΟΦΟΡΙΚΗΣ 19/5/2007
Οδηγίες: Να απαντηθούν όλες οι ερωτήσεις. Αν κάπου κάνετε κάποιες υποθέσεις να αναφερθούν στη σχετική ερώτηση. Όλα τα αρχεία που αναφέρονται στα προβλήματα βρίσκονται στον ίδιο φάκελο με το εκτελέσιμο
Διαβάστε περισσότεραComparison of Evapotranspiration between Indigenous Vegetation and Invading Vegetation in a Bog
J. Jpn. Soc. Soil Phys. No. +*-, p.-3.1,**0 ** * *** Comparison of Evapotranspiration between Indigenous Vegetation and Invading Vegetation in a Bog Toshiki FUJIMOTO*, Ippei IIYAMA*, Mai SAKAI*, Osamu
Διαβάστε περισσότεραΔΗΜΟΣΙΕΥΣΗ Νο 56 ΠΡΑΚΤΙΚΑ 5 ΟΥ ΠΑΝΕΛΛΗΝΙΟΥ ΓΕΩΓΡΑΦΙΚΟΥ ΣΥΝΕΔΡΙΟΥ
ΔΗΜΟΣΙΕΥΣΗ Νο 56 ΠΡΑΚΤΙΚΑ 5 ΟΥ ΠΑΝΕΛΛΗΝΙΟΥ ΓΕΩΓΡΑΦΙΚΟΥ ΣΥΝΕΔΡΙΟΥ ΜΑΡΙΟΛΑΚΟΣ, Η., ΑΛΕΞΟΠΟΥΛΟΣ, Ι., ΠΑΠΑΔΟΠΟΥΛΟΣ, Τ., ΦΟΥΝΤΟΥΛΗΣ, Ι. (1999). - Γεωμορφολογική δομή της πόλγης της Πολιανής (Ν. Μεσσηνίας) με
Διαβάστε περισσότεραNumerical Analysis FMN011
Numerical Analysis FMN011 Carmen Arévalo Lund University carmen@maths.lth.se Lecture 12 Periodic data A function g has period P if g(x + P ) = g(x) Model: Trigonometric polynomial of order M T M (x) =
Διαβάστε περισσότεραTwo-ship Seismic Reflection Profiling Across the Source Area of the,**1 Noto Hanto Earthquake, Central Japan
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2,,**1 pp.,1/,33,**1 * +, - +,, + -, Two-ship Seismic Reflection Profiling Across the Source Area of the,**1 Noto Hanto Earthquake, Central Japan Hiroshi Sato
Διαβάστε περισσότεραMEMS. Evaluation of MEMS Accelerometer Sensor for Earthquake
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2.,**3 pp.,/+,00 MEMS * +, +, + +, Evaluation of MEMS Accelerometer Sensor for Earthquake Observations Fumitoshi Murakami *, Hiroshi Sato, Toru Kuroda, Susumu
Διαβάστε περισσότεραCHAPTER 12: PERIMETER, AREA, CIRCUMFERENCE, AND 12.1 INTRODUCTION TO GEOMETRIC 12.2 PERIMETER: SQUARES, RECTANGLES,
CHAPTER : PERIMETER, AREA, CIRCUMFERENCE, AND SIGNED FRACTIONS. INTRODUCTION TO GEOMETRIC MEASUREMENTS p. -3. PERIMETER: SQUARES, RECTANGLES, TRIANGLES p. 4-5.3 AREA: SQUARES, RECTANGLES, TRIANGLES p.
Διαβάστε περισσότεραΤΕΧΝΟΛΟΓΙΚΟ ΕΚΠΑΙ ΕΥΤΙΚΟ Ι ΡΥΜΑ ΚΡΗΤΗΣ ΤΜΗΜΑ ΦΥΣΙΚΩΝ ΠΟΡΩΝ & ΠΕΡΙΒΑΛΛΟΝΤΟΣ ΤΟΜΕΑΣ ΠΕΡΙΒΑΛΛΟΝΤΙΚΗΣ ΤΕΧΝΟΛΟΓΙΑΣ ΕΡΓΑΣΤΗΡΙΟ ΕΛΕΓΧΟΥ ΠΟΙΟΤΗΤΑΣ Υ ΑΤΙΚΩΝ & Ε ΑΦΙΚΩΝ ΠΟΡΩΝ ΕΠΙΒΑΡΥΝΣΗ ΜΕ ΒΑΡΕΑ ΜΕΤΑΛΛΑ Ε ΑΦΩΝ ΤΗΣ
Διαβάστε περισσότεραShallow P-wave Velocity Structure of Shirane Pyroclastic Cone, Kusatsu-Shirane Volcano Derived from a Controlled Seismic Experiment
/* (,**/) + 3 +0 P,**. 1,+,**. +, +* Shallow P-wave Velocity Structure of Shirane Pyroclastic Cone, Kusatsu-Shirane Volcano Derived from a Controlled Seismic Experiment Shin ya ONIZAWA, Takehiko MORI,
Διαβάστε περισσότεραChapter 7 Transformations of Stress and Strain
Chapter 7 Transformations of Stress and Strain INTRODUCTION Transformation of Plane Stress Mohr s Circle for Plane Stress Application of Mohr s Circle to 3D Analsis 90 60 60 0 0 50 90 Introduction 7-1
Διαβάστε περισσότεραStudy of In-vehicle Sound Field Creation by Simultaneous Equation Method
Study of In-vehicle Sound Field Creation by Simultaneous Equation Method Kensaku FUJII Isao WAKABAYASI Tadashi UJINO Shigeki KATO Abstract FUJITSU TEN Limited has developed "TOYOTA remium Sound System"
Διαβάστε περισσότεραGPS observations on the Antarctic ice sheet conducted during JARE-.+
7 Scientific Note.+ GPS + +, - GPS observations on the Antarctic ice sheet conducted during JARE-.+ Koichiro Doi +, Naoya Imae +, Naoyosi Iwata, and Noritsune Seo -,**- +* 1 ;,**- +, - Abstract: We conducted
Διαβάστε περισσότεραΓεωλογικά Γεωτεχνικά Προβλήματα που Απαντώνται σε Θεμελιώσεις Τεχνικών Έργων Παρά τα Ρήγματα
4 ο Πανελλήνιο συνέδριο Γεωτεχνικής και Γεωπεριβαλλοντικής Μηχανικής, ΤΕΕ Ελληνική Επιστημονική Εταιρία Εδαφομηχανικής και Θεμελιώσεων, Αθήνα 2001, τομ.2, 193-200. Γεωλογικά Γεωτεχνικά Προβλήματα που Απαντώνται
Διαβάστε περισσότεραIkuo Hara*and Takami Miyamoto**
.1 + +,,**- Japanese Journal of Structural Geology, No..1, + +,,,**- Some Considerations on the Research History of the Paleo-Ryoke Belt (-) The Median Tectonic Line of Pre-Ichinokawa Stage * ** Ikuo Hara*and
Διαβάστε περισσότερα«ΧΩΡΙΚΗ ΜΟΝΤΕΛΟΠΟΙΗΣΗ ΤΗΣ ΚΑΤΑΝΟΜΗΣ ΤΟΥ ΠΛΗΘΥΣΜΟΥ ΤΗΣ ΠΕΡΔΙΚΑΣ (ALECTORIS GRAECA) ΣΤΗ ΣΤΕΡΕΑ ΕΛΛΑΔΑ»
ΓΕΩΠΟΝΙΚΟ ΠΑΝΕΠΙΣΤΗΜΕΙΟ ΑΘΗΝΩΝ ΤΜΗΜΑ ΑΞΙΟΠΟΙΗΣΗΣ ΦΥΣΙΚΩΝ ΠΟΡΩΝ & ΓΕΩΡΓΙΚΗΣ ΜΗΧΑΝΙΚΗΣ ΠΡΟΓΡΑΜΜΑ ΜΕΤΑΠΤΥΧΙΑΚΩΝ ΣΠΟΥΔΩΝ ΕΙΔΙΚΕΥΣΗ: ΕΔΑΡΜΟΓΕΣ ΤΗΣ ΓΕΩΠΛΗΡΟΦΟΡΙΚΗΣ ΣΤΟΥΣ ΦΥΣΙΚΟΥΣ ΠΟΡΟΥΣ «ΧΩΡΙΚΗ ΜΟΝΤΕΛΟΠΟΙΗΣΗ
Διαβάστε περισσότεραE#ects of Drying on Bacterial Activity and Iron Formation in Acid Sulfate Soils
J. Jpn. Soc. Soil Phys. No. 3+, p..3 /1,**, * ** ** E#ects of Drying on Bacterial Activity and Iron Formation in Acid Sulfate Soils Kaoru UENO*, Tadashi ADACHI** and Hajime NARIOKA** * The Graduate School
Διαβάστε περισσότεραAppendix to On the stability of a compressible axisymmetric rotating flow in a pipe. By Z. Rusak & J. H. Lee
Appendi to On the stability of a compressible aisymmetric rotating flow in a pipe By Z. Rusak & J. H. Lee Journal of Fluid Mechanics, vol. 5 4, pp. 5 4 This material has not been copy-edited or typeset
Διαβάστε περισσότερα( ) , ) , ; kg 1) 80 % kg. Vol. 28,No. 1 Jan.,2006 RESOURCES SCIENCE : (2006) ,2 ,,,, ; ;
28 1 2006 1 RESOURCES SCIENCE Vol. 28 No. 1 Jan. 2006 :1007-7588(2006) 01-0002 - 07 20 1 1 2 (11 100101 ; 21 101149) : 1978 1978 2001 ; 2010 ; ; ; : ; ; 24718kg 1) 1990 26211kg 260kg 1995 2001 238kg( 1)
Διαβάστε περισσότεραCHAPTER 25 SOLVING EQUATIONS BY ITERATIVE METHODS
CHAPTER 5 SOLVING EQUATIONS BY ITERATIVE METHODS EXERCISE 104 Page 8 1. Find the positive root of the equation x + 3x 5 = 0, correct to 3 significant figures, using the method of bisection. Let f(x) =
Διαβάστε περισσότεραP- and S-Wave Seismic Reflection Profiling Across the Kamishiro Fault, Itoigawa-Shizuoka Tectonic Line Active Fault System, Central Japan
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2,,**1 pp.,/ -/ +, -. / 0 1 2 3 - +* +* ++ +, +- +. +/ +0 +1 - +2 +3,* -,+ + :, -. : / 0 : 1 : 2 3 +* ++ +, +- +. : +/ : +0 : +1 : +2 : +3 :,* :,+ P- and S-Wave
Διαβάστε περισσότεραΔΙΠΛΩΜΑΤΙΚΗ ΕΡΓΑΣΙΑ ΕΠΑΝΑΣΧΕΔΙΑΣΜΟΣ ΓΡΑΜΜΗΣ ΣΥΝΑΡΜΟΛΟΓΗΣΗΣ ΜΕ ΧΡΗΣΗ ΕΡΓΑΛΕΙΩΝ ΛΙΤΗΣ ΠΑΡΑΓΩΓΗΣ REDESIGNING AN ASSEMBLY LINE WITH LEAN PRODUCTION TOOLS
ΔΙΑΤΜΗΜΑΤΙΚΟ ΠΡΟΓΡΑΜΜΑ ΜΕΤΑΠΤΥΧΙΑΚΩΝ ΣΠΟΥΔΩΝ ΣΤΗ ΔΙΟΙΚΗΣΗ ΤΩΝ ΕΠΙΧΕΙΡΗΣΕΩΝ ΔΙΠΛΩΜΑΤΙΚΗ ΕΡΓΑΣΙΑ ΕΠΑΝΑΣΧΕΔΙΑΣΜΟΣ ΓΡΑΜΜΗΣ ΣΥΝΑΡΜΟΛΟΓΗΣΗΣ ΜΕ ΧΡΗΣΗ ΕΡΓΑΛΕΙΩΝ ΛΙΤΗΣ ΠΑΡΑΓΩΓΗΣ REDESIGNING AN ASSEMBLY LINE WITH
Διαβάστε περισσότεραΘωμάς ΣΑΛΟΝΙΚΙΟΣ 1, Χρήστος ΚΑΡΑΚΩΣΤΑΣ 2, Βασίλειος ΛΕΚΙΔΗΣ 2, Μίλτων ΔΗΜΟΣΘΕΝΟΥΣ 1, Τριαντάφυλλος ΜΑΚΑΡΙΟΣ 3,
Αξιοποίηση Έξι Σεισμών στην Πελοπόννησο για την Συσχέτιση Φασματικών Επιταχύνσεων με την Απόκριση του Δομημένου Περιβάλλοντος Correlation of Spectral Accelerations with the Response of the Built Environment
Διαβάστε περισσότεραSpherical Coordinates
Spherical Coordinates MATH 311, Calculus III J. Robert Buchanan Department of Mathematics Fall 2011 Spherical Coordinates Another means of locating points in three-dimensional space is known as the spherical
Διαβάστε περισσότεραFigure 3 Three observations (Vp, Vs and density isosurfaces) intersecting in the PLF space. Solutions exist at the two indicated points.
φ φ φ φ Figure 1 Resampling of a rock-physics model from velocity-porosity to lithology-porosity space. C i are model results for various clay contents. φ ρ ρ δ Figure 2 Bulk modulus constraint cube in
Διαβάστε περισσότερα12 2006 Journal of the Institute of Science and Engineering. Chuo University
12 2006 Journal of the Institute of Science and Engineering. Chuo University abstract In order to study the mitigation effect on urban heated environment of urban park, the microclimate observations have
Διαβάστε περισσότεραGround Tilt Change Associated with the,**. Eruption at Asamayama Volcano, Japan
/+ (,**0) + 3+ +*+,**.,**/ / +0,**0 + +0 Ground Tilt Change Associated with the,**. Eruption at Asamayama Volcano, Japan Masaaki CHUREI and Hiroaki KATAYAMA The eruptive activity of Asamayama Volcano started
Διαβάστε περισσότεραConductivity Logging for Thermal Spring Well
/.,**. 25 +,1- **-- 0/2,,,1- **-- 0/2, +,, +/., +0 /,* Conductivity Logging for Thermal Spring Well Koji SATO +, Tadashi TAKAYA,, Tadashi CHIBA, + Nihon Chika Kenkyuusho Co. Ltd., 0/2,, Hongo, Funabashi,
Διαβάστε περισσότερα22 .5 Real consumption.5 Real residential investment.5.5.5 965 975 985 995 25.5 965 975 985 995 25.5 Real house prices.5 Real fixed investment.5.5.5 965 975 985 995 25.5 965 975 985 995 25.3 Inflation
Διαβάστε περισσότεραAΡΙΣΤΟΤΕΛΕΙΟ ΠΑΝΕΠΙΣΤΗΜΙΟ ΘΕΣΣΑΛΟΝΙΚΗΣ ΠΟΛΥΤΕΧΝΙΚΗ ΣΧΟΛΗ ΤΜΗΜΑ ΠΟΛΙΤΙΚΩΝ ΜΗΧΑΝΙΚΩΝ
AΡΙΣΤΟΤΕΛΕΙΟ ΠΑΝΕΠΙΣΤΗΜΙΟ ΘΕΣΣΑΛΟΝΙΚΗΣ ΠΟΛΥΤΕΧΝΙΚΗ ΣΧΟΛΗ ΤΜΗΜΑ ΠΟΛΙΤΙΚΩΝ ΜΗΧΑΝΙΚΩΝ ΠΡΟΓΡΑΜΜΑ ΜΕΤΑΠΤΥΧΙΑΚΩΝ ΣΠΟΥΔΩΝ ΕΙΔΙΚΕΥΣΗΣ ΠΡΟΣΤΑΣΙΑ ΠΕΡΙΒΑΛΛΟΝΤΟΣ ΚΑΙ ΒΙΩΣΙΜΗ ΑΝΑΠΤΥΞΗ ΔΙΕΡΕΥΝΗΣΗ ΤΩΝ ΠΙΕΣΕΩΝ ΣΤΟ ΠΕΡΙΒΑΛΛΟΝ
Διαβάστε περισσότεραΠΑΝΕΠΙΣΤΗΜΙΟ ΠΑΤΡΩΝ ΤΜΗΜΑ ΗΛΕΚΤΡΟΛΟΓΩΝ ΜΗΧΑΝΙΚΩΝ ΚΑΙ ΤΕΧΝΟΛΟΓΙΑΣ ΥΠΟΛΟΓΙΣΤΩΝ ΤΟΜΕΑΣ ΣΥΣΤΗΜΑΤΩΝ ΗΛΕΚΤΡΙΚΗΣ ΕΝΕΡΓΕΙΑΣ
ΠΑΝΕΠΙΣΤΗΜΙΟ ΠΑΤΡΩΝ ΤΜΗΜΑ ΗΛΕΚΤΡΟΛΟΓΩΝ ΜΗΧΑΝΙΚΩΝ ΚΑΙ ΤΕΧΝΟΛΟΓΙΑΣ ΥΠΟΛΟΓΙΣΤΩΝ ΤΟΜΕΑΣ ΣΥΣΤΗΜΑΤΩΝ ΗΛΕΚΤΡΙΚΗΣ ΕΝΕΡΓΕΙΑΣ Διπλωματική Εργασία του φοιτητή του τμήματος Ηλεκτρολόγων Μηχανικών και Τεχνολογίας Ηλεκτρονικών
Διαβάστε περισσότεραA,.* Ma Widespread Tephra Associated with a Large-Scale Pyroclastic Flow from the Sengan Geothermal Area, Northeast Japan Arc
/, (,**1) +,- -2,.* Ma,**0 0,-,**0 +,,, A,.* Ma Widespread Tephra Associated with a Large-Scale Pyroclastic Flow from the Sengan Geothermal Area, Northeast Japan Arc Takehiko SUZUKI and Toshio NAKAYAMA
Διαβάστε περισσότεραΕυθύμης ΛΕΚΚΑΣ 1. 3 o Πανελλήνιο Συνέδριο Αντισεισμικής Μηχανικής & Τεχνικής Σεισμολογίας 5 7 Νοεμβρίου, 2008 Άρθρο 2109
3 o Πανελλήνιο Συνέδριο Αντισεισμικής Μηχανικής & Τεχνικής Σεισμολογίας 5 7 Νοεμβρίου, 2008 Άρθρο 2109 Σεισμός Wenchuan (Mw 7.9, 12 Μαΐου 2008) Sichuan, Κίνα. Γεωτεκτονικό Καθεστώς και Μακρο-κατανομή των
Διαβάστε περισσότεραToward the Quantitative Study of Hydrothermal Systems An Approach to Understand Hydrothermal Systems
J. Hot Spring Sci. 0*,0+,1+,*+* + Toward the Quantitative Study of Hydrothermal Systems An Approach to Understand Hydrothermal Systems Sachio E + HARA Abstract The quantitative understanding of hydrothermal
Διαβάστε περισσότεραHigh-Resolution P-wave Seismic Reflection Imaging of the Suzuka Basement-Involved Fold:,**/ Tokiyama Profile
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2,,**1 pp. 3/ +*- P :,**/ + *, -. / 0 1 2 3 +* ++ +, +- +. + :, -. : / : 0 : 1 2 3 : +* ++ +, : +- : +. : High-Resolution P-wave Seismic Reflection Imaging of
Διαβάστε περισσότεραkatoh@kuraka.co.jp okaken@kuraka.co.jp mineot@fukuoka-u.ac.jp 4 35 3 Normalized stress σ/g 25 2 15 1 5 Breaking test Theory 1 2 Shear tests Failure tests Compressive tests 1 2 3 4 5 6 Fig.1. Relation between
Διαβάστε περισσότεραQuantitative chemical analyses of rocks with X-ray fluorescence analyzer: major and trace elements in ultrabasic rocks
98 Scientific Note X : Quantitative chemical analyses of rocks with X-ray fluorescence analyzer: major and trace elements in ultrabasic rocks Kimiko Seno and Yoichi Motoyoshi,**- +, +, ;,**. -,/ Abstract:
Διαβάστε περισσότεραMean bond enthalpy Standard enthalpy of formation Bond N H N N N N H O O O
Q1. (a) Explain the meaning of the terms mean bond enthalpy and standard enthalpy of formation. Mean bond enthalpy... Standard enthalpy of formation... (5) (b) Some mean bond enthalpies are given below.
Διαβάστε περισσότεραThe origin of the Canary Island Seamount Province New ages of old seamounts. Paul van den Bogaard. Supplementary information
The origin of the Canary Island Seamount Province New ages of old seamounts. Paul van den Bogaard Supplementary information Supplementary information S1: Major CISP seamount coordinates Longitude Latitude
Διαβάστε περισσότεραReview of Previous Studies on M 1-class that Occurred in the Southern Kanto Region and Data Collection
Bull Earthq Res Inst Univ Tokyo Vol 2,**3 pp +2-,+, M 1 +3,+ +3,, +321 * +, + + +, Review of Previous Studies on M 1-class Earthquakes that Occurred in the Southern Kanto Region and Data Collection The
Διαβάστε περισσότεραΠΕΡΙΕΧΟΜΕΝΑ. Κεφάλαιο 1: Κεφάλαιο 2: Κεφάλαιο 3:
4 Πρόλογος Η παρούσα διπλωµατική εργασία µε τίτλο «ιερεύνηση χωρικής κατανοµής µετεωρολογικών µεταβλητών. Εφαρµογή στον ελληνικό χώρο», ανατέθηκε από το ιεπιστηµονικό ιατµηµατικό Πρόγραµµα Μεταπτυχιακών
Διαβάστε περισσότεραVol. 31,No JOURNAL OF CHINA UNIVERSITY OF SCIENCE AND TECHNOLOGY Feb
Ξ 31 Vol 31,No 1 2 0 0 1 2 JOURNAL OF CHINA UNIVERSITY OF SCIENCE AND TECHNOLOGY Feb 2 0 0 1 :025322778 (2001) 0120016205 (, 230026) : Q ( m 1, m 2,, m n ) k = m 1 + m 2 + + m n - n : Q ( m 1, m 2,, m
Διαβάστε περισσότεραDepartment of Earth & Planetary Science, the University of Tokyo, - Department of Geology Earth material science, Niigata University,
Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2*,**/ pp. + 3,**. : + * +, + -. / 0-1 2 3. 1, 2 +* +* +* +, -. / 0 1 2 3 +* High-resolution seismic reflection profiling across the surface rupture associated
Διαβάστε περισσότερα,*+* .* +/* +* -* ac. jp +3, *
The Quaternary Research /+, p 0/ 12,*+,,*+* : * * +/* +* -* : I, +,* II,*++ +, +3,*+,, ++ * +3, *-31 + + E-mail : suzukit@tmu ac jp 66 /+, +, AdV : BnV : NmC : SnC : NrToOnC : NsV : SoC : TkV : NyV : NtV
Διαβάστε περισσότεραTable of Contents 1 Supplementary Data MCD
Electronic Supplementary Material (ESI) for Dalton Transactions. This journal is The Royal Society of Chemistry 2017 Supporting Information for Magnetic circular dichroism and density functional theory
Διαβάστε περισσότεραΠΑΝΕΠΙΣΤΗΜΙΟ ΠΑΤΡΩΝ ΤΜΗΜΑ ΗΛΕΚΤΡΟΛΟΓΩΝ ΜΗΧΑΝΙΚΩΝ ΚΑΙ ΤΕΧΝΟΛΟΓΙΑΣ ΥΠΟΛΟΓΙΣΤΩΝ ΤΟΜΕΑΣ ΣΥΣΤΗΜΑΤΩΝ ΗΛΕΚΤΡΙΚΗΣ ΕΝΕΡΓΕΙΑΣ
ΠΑΝΕΠΙΣΤΗΜΙΟ ΠΑΤΡΩΝ ΤΜΗΜΑ ΗΛΕΚΤΡΟΛΟΓΩΝ ΜΗΧΑΝΙΚΩΝ ΚΑΙ ΤΕΧΝΟΛΟΓΙΑΣ ΥΠΟΛΟΓΙΣΤΩΝ ΤΟΜΕΑΣ ΣΥΣΤΗΜΑΤΩΝ ΗΛΕΚΤΡΙΚΗΣ ΕΝΕΡΓΕΙΑΣ ιπλωµατική Εργασία του φοιτητή του τµήµατος Ηλεκτρολόγων Μηχανικών και Τεχνολογίας Ηλεκτρονικών
Διαβάστε περισσότεραDevelopment of a Seismic Data Analysis System for a Short-term Training for Researchers from Developing Countries
No. 2 3+/,**, Technical Research Report, Earthquake Research Institute, University of Tokyo, No. 2, pp.3+/,,**,. * * Development of a Seismic Data Analysis System for a Short-term Training for Researchers
Διαβάστε περισσότεραMath 6 SL Probability Distributions Practice Test Mark Scheme
Math 6 SL Probability Distributions Practice Test Mark Scheme. (a) Note: Award A for vertical line to right of mean, A for shading to right of their vertical line. AA N (b) evidence of recognizing symmetry
Διαβάστε περισσότεραΚΛΙΜΑΤΟΛΟΓΙΑ CLIMATOLOGY
10 ο COMECAP 2010, Πρακτικά Συνεδρίου, Πάτρα 10 th COMECAP 2010, Proceedings, Patras, Greece ΚΛΙΜΑΤΟΛΟΓΙΑ CLIMATOLOGY ΥΧΡΟΥΡΟΝΗΚΖ ΓΗΑΚΤΜΑΝΖ ΣΧΝ ΖΛΔΚΣΡΗΚΧΝ ΔΚΚΔΝΧΔΧΝ ΣΖΝ ΔΛΛΑΓΑ ΓΗΑ ΣΖΝ ΥΡΟΝΗΚΖ ΠΔΡΗΟΓΟ 1998-2007
Διαβάστε περισσότεραParametrized Surfaces
Parametrized Surfaces Recall from our unit on vector-valued functions at the beginning of the semester that an R 3 -valued function c(t) in one parameter is a mapping of the form c : I R 3 where I is some
Διαβάστε περισσότεραHIV HIV HIV HIV AIDS 3 :.1 /-,**1 +332
,**1 The Japanese Society for AIDS Research The Journal of AIDS Research +,, +,, +,, + -. / 0 1 +, -. / 0 1 : :,**- +,**. 1..+ - : +** 22 HIV AIDS HIV HIV AIDS : HIV AIDS HIV :HIV AIDS 3 :.1 /-,**1 HIV
Διαβάστε περισσότεραAreas and Lengths in Polar Coordinates
Kiryl Tsishchanka Areas and Lengths in Polar Coordinates In this section we develop the formula for the area of a region whose boundary is given by a polar equation. We need to use the formula for the
Διαβάστε περισσότεραAreas and Lengths in Polar Coordinates
Kiryl Tsishchanka Areas and Lengths in Polar Coordinates In this section we develop the formula for the area of a region whose boundary is given by a polar equation. We need to use the formula for the
Διαβάστε περισσότεραPhysical and Chemical Properties of the Nest-site Beach of the Horseshoe Crab Rehabilitated by Sand Placement
J. Jpn. Soc. Soil Phys. No. 33, p.//0-,**/ ******* * Physical and Chemical Properties of the Nest-site Beach of the Horseshoe Crab Rehabilitated by Sand Placement Masami OHTSUBO*, Hidekazu ISHIDA**, Hisakatsu
Διαβάστε περισσότεραPhysicsAndMathsTutor.com 1
PhysicsAndMathsTutor.com 1 Q1. The magnetic flux through a coil of N turns is increased uniformly from zero to a maximum value in a time t. An emf, E, is induced across the coil. What is the maximum value
Διαβάστε περισσότεραSection 9.2 Polar Equations and Graphs
180 Section 9. Polar Equations and Graphs In this section, we will be graphing polar equations on a polar grid. In the first few examples, we will write the polar equation in rectangular form to help identify
Διαβάστε περισσότερα1(a) moat. moat. moat. 1(b) moving magnetic feature
High Altitude Observatory, National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307 3000, USA e-mail: kubo@ucar.edu 1. km km 1 2 100 1) 2. 1(a) moat moat 1(a) moat 1(b) moat moat moat
Διαβάστε περισσότεραΑστικές παρεμβάσεις ανάπλασης αδιαμόρφωτων χώρων. Δημιουργία βιώσιμου αστικού περιβάλλοντος και σύνδεση τριών κομβικών σημείων στην πόλη της Δράμας
ΤΕΙ ΚΑΒΑΛΑΣ ΠΑΡΑΡΤΗΜΑ ΔΡΑΜΑΣ ΤΜΗΜΑ ΑΡΧΙΤΕΚΤΟΝΙΚΗΤΟΠΙΟΥ Αστικές παρεμβάσεις ανάπλασης αδιαμόρφωτων χώρων. Δημιουργία βιώσιμου αστικού περιβάλλοντος και σύνδεση τριών κομβικών σημείων στην πόλη της Δράμας
Διαβάστε περισσότεραNeutralization E#ects of Acidity of Rain by Cover Plants on Slope Land
J. Jpn. Soc. Soil Phys. No. 33, p.2/ 3.,**/ * * * ** Neutralization E#ects of Acidity of Rain by Cover Plants on Slope Land Tadashi ADACHI*, Yoko OKI*, Akihiro NAGAI* and Shogo NAKATSUKASA** * Faculty
Διαβάστε περισσότεραΗΜΕΡΙΔΑ ΕΠΙΤΡΟΠΗΣ ΤΕΚΤΟΝΙΚΗΣ Ε.Γ.Ε
Tectonic ΗΜΕΡΙΔΑ evolution of the External Hellenides Department of Geology, University of Patras, Greece Koukouvelas I., Kokkalas S., Xypolias P. The Hellenides and previous models Parnassos Zone Pelagonian
Διαβάστε περισσότεραBEHAVIOR OF MASSIVE EARTH RETAINING WALLS UNDER EARTHQUAKE SHAKING Comparisons to EC-8 Provisions
UNIVERSITY OF PATRAS DEPARTMENT OF CIVIL ENGINEERING Laboratory of Geotechnical Engineering BEHAVIOR OF MASSIVE EARTH RETAINING WALLS UNDER EARTHQUAKE SHAKING Comparisons to EC-8 Provisions Prof. G. Athanasopoulos
Διαβάστε περισσότερα«ΑΓΡΟΤΟΥΡΙΣΜΟΣ ΚΑΙ ΤΟΠΙΚΗ ΑΝΑΠΤΥΞΗ: Ο ΡΟΛΟΣ ΤΩΝ ΝΕΩΝ ΤΕΧΝΟΛΟΓΙΩΝ ΣΤΗΝ ΠΡΟΩΘΗΣΗ ΤΩΝ ΓΥΝΑΙΚΕΙΩΝ ΣΥΝΕΤΑΙΡΙΣΜΩΝ»
I ΑΡΙΣΤΟΤΕΛΕΙΟ ΠΑΝΕΠΙΣΤΗΜΙΟ ΘΕΣΣΑΛΟΝΙΚΗΣ ΣΧΟΛΗ ΝΟΜΙΚΩΝ ΟΙΚΟΝΟΜΙΚΩΝ ΚΑΙ ΠΟΛΙΤΙΚΩΝ ΕΠΙΣΤΗΜΩΝ ΤΜΗΜΑ ΟΙΚΟΝΟΜΙΚΩΝ ΕΠΙΣΤΗΜΩΝ ΠΡΟΓΡΑΜΜΑ ΜΕΤΑΠΤΥΧΙΑΚΩΝ ΣΠΟΥΔΩΝ ΣΤΗΝ «ΔΙΟΙΚΗΣΗ ΚΑΙ ΟΙΚΟΝΟΜΙΑ» ΚΑΤΕΥΘΥΝΣΗ: ΟΙΚΟΝΟΜΙΚΗ
Διαβάστε περισσότεραMolecular evolutionary dynamics of respiratory syncytial virus group A in
Molecular evolutionary dynamics of respiratory syncytial virus group A in recurrent epidemics in coastal Kenya James R. Otieno 1#, Charles N. Agoti 1, 2, Caroline W. Gitahi 1, Ann Bett 1, Mwanajuma Ngama
Διαβάστε περισσότεραHomework 8 Model Solution Section
MATH 004 Homework Solution Homework 8 Model Solution Section 14.5 14.6. 14.5. Use the Chain Rule to find dz where z cosx + 4y), x 5t 4, y 1 t. dz dx + dy y sinx + 4y)0t + 4) sinx + 4y) 1t ) 0t + 4t ) sinx
Διαβάστε περισσότεραis like multiplying by the conversion factor of. Dividing by 2π gives you the
Chapter Graphs of Trigonometric Functions Answer Ke. Radian Measure Answers. π. π. π. π. 7π. π 7. 70 8. 9. 0 0. 0. 00. 80. Multipling b π π is like multipling b the conversion factor of. Dividing b 0 gives
Διαβάστε περισσότερα