Journal of asian earth sciences pdf

Journal of asian earth sciences pdf
helping to create an assessment of the geothermal potential for electric generation from the Hammam Faraun hot spring. Previous studies have been conducted on the geological and
et al., 2008a,b; Chen et al., 2010, 2012a). The development of the Cenozoic contractional structures may have been induced by southward subduction of the Asian lithosphere underneath the
well as a possible gap in earthquakes above the Pingtung event). The occurrence of strike-slip events is expected given the 3D defor-mation of Taiwan (and possible southward migration of deforma-
terrains of the Indus River system when a given river drains only a single source terrain. This technique was used to constrain the source of the sediment in the modern stream and to compare this
Middle–Upper Permian carbon isotope stratigraphy at Chaotian, South China: Pre-extinction multiple upwelling of oxygen-depleted water onto continental shelf
2. Geological setting and petrography The jadeite uplift (Fig. 1) containing the Myanmar jadeite deposit and high-pressure rocks in Hpakan area of Kachin State
climate anomalies. In Pausata et al. (2011), the model result showed that a sudden cooling in the Northern Hemisphere caused by an increase in North Atlantic sea-ice during the last glacial per-
Shallow crustal and intermediate-depth events with 4.0 > M P 2.0 that occurred between February and July, 2006, recorded at 189 Hi-net seismic stations in SW Japan have been
Molchan and Kagan, 1992), which motivates us to carry out the statistical analysis examining the SIPs of GPS TEC in China. In this study, GIM TECs are investigated for 56 M P 6.0 earth-

expressed as a function of the V P/V S ratio in the medium. The Wad-atianalysis is based on P and Sarrivaltimedifferencesas a function of P arrival times.
Earthquake potential of the Sichuan-Yunnan region, western China Fan Wanga,b, Min Wanga, Yanzhao Wanga, Zheng-Kang Shenc,d,⇑ a State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
are evaluated using available trace elements and Re–Os and S iso-tope geochemical evidence. 2. Regional geology The CAOB is a Late Paleozoic orogenic belt from the Siberian
Geochronology and geochemistry of Late Devonian and early Carboniferous igneous rocks of central Jilin Province, NE China: Implications for the tectonic evolution of the eastern Central Asian
Differential destruction of the North China Craton: A tectonic perspective Yan-Jie Tanga,⇑, Hong-Fu Zhanga,b, M. Santoshc, Ji-Feng Yinga a State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China

Journal of Asian Earth Sciences core.ac.uk




Journal of Asian Earth Sciences 中国科学院

Malaysia. The studied succession displays a wide range of facies and facies successions, with evidence for deposition by fluvial-, wave-, and tide-generated processes.
Geological variation in S-wave velocity structures in Northern Taiwan and implications for seismic hazards based on ambient noise analysis Ya-Chuan Laia,⇑, Bor-Shouh Huanga, Yu-Chih Huanga,b, Huajian Yaoc, Ruey-Der Hwangd,
The shear-wave splitting in the crust and the upper mantle around the Bohai Sea, North China Shi Yutao⇑, Gao Yuan, Tai Lingxue, Fu Yuanyuan Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, PR China
152 Y.H. Dawood et al./Journal of Asian Earth Sciences 77 (2013) 151–162 represented from the east to the west by the Precambrian base- ment rocks that were unconformably overlain by Tertiary sedi-
Paleomagnetism of the late Cryogenian Nantuo Formation and paleogeographic implications for the South China Block Shihong Zhanga,⇑, David A.D. Evansb, Haiyan Lia, Huaichun Wua, Ganqing Jiangc, Jin …
The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology , tectonics , geochemistry and geophysics of Asia.
bDepartment of Earth and Space Science, University of California, Los Angeles, CA 90095, USA c Geo- and Atmospheric Sciences, University of Innsbruck, Innsbruck, Austria d Institute of Geomechanics, Chinese Academy of Geology Sciences, Beijing, China
Moyra E.J. Wilson Senior Lecturer, Earth Sciences, University of Western Australia (UWA), Perth, Australia Verified email at uwa.edu.au Chris Morley Petroleum Geophysics MSc Program, Chiang Mai University, Chiang Mai, Thailand


Read the latest articles of Journal of Southeast Asian Earth Sciences at ScienceDirect.com, Elsevier’s leading platform of peer-reviewed scholarly literature
Nitrogen isotope chemostratigraphy across the Permian–Triassic boundary at Chaotian, Sichuan, South China Masafumi Saitoha,b,⇑, Yuichiro Uenoa,c, Manabu
surface or the axial plane cleavage varies within the domain, and is consistent with the sinuous hinge lines on the geologic map. At the outcrop level, variation in the dip angle of fold hinge lines is com-


G. Zhang et al./Journal of Asian Earth Sciences 35 (2009) 310–322 311 is a large lensoid block, about 800 m wide and 1700 m long (Fig. 1c), enclosing the serpentinized harzburgite (Fig. 2c).
Editorial The 2008 Wenchuan earthquake and active tectonics of Asia 1. Introduction The great Wenchuan earthquake (Mw 7.9 or Ms 8.0), struck western …
A few earthquake conundrums resolved Stuart Crampina,b,⇑, Yuan Gaoc, Angelo De Santisd,e a British Geological Survey, Edinburgh, Scotland, UK bAlso at School of …
Burchfiel and Chen, 2012). The Sichuan Basin, occupying the north-western part of the Yangtze carton, lying on the east of the LMF, is considered as an elongate and moderately deformed peripheral
2 D.K. Bora et al./Journal of Asian Earth Sciences 90 (2014) 1–14 the Himalayan collision zone to the north and from the Indo- Burma subduction zone to the east, the Shillong Plateau has a his-
Journal of Asian Earth Sciences Review Articles Recently published review articles from Journal of Asian Earth Sciences Review Articles The Sipoholon Geothermal Field and adjacent geothermal systems along the North-Central Sumatra Fault Belt, Indonesia: Reviews on geochemistry, tectonics, and natural heat loss
effort has been devoted to estimate differences between SH-wave velocity and SV-wave velocity both regionally (Villasenˇor et al., 2001) and globally (Shapiro and Ritzwoller, 2002).
regional velocity model for depth conversions. The subsurface data are used here specifically to determine relative life-spans and ages of faults.



Journal of Asian Earth Sciences igg.cas.cn

2 J. Zhao et al./Journal of Asian Earth Sciences xxx (2015) xxx–xxx Please cite this article in press as: Zhao, J., et al. Late Triassic paleomagnetic result from the Baoshan Terrane, West
Precambrian crustal evolution of Peninsular India: A 3.0 billion year odyssey Joseph G. Meerta,*, Manoj K. Panditb, Vimal R. Pradhana, Jonathan Banksa, Robert
craton destruction should use geophysical methods that can deter-mine the water content of the mantle. Magnetotellurics is one such method and is used in this paper.
Tsunami hazard from the subduction megathrust of the South China Sea: Part I. Source characterization and the resulting tsunami Kusnowidjaja Megawatia,b,*, Felicia …
Geochemical and isotopic constraints on the evolution of Late Paleozoic dyke swarms in West Junggar, Xinjiang, China Yan Zhana, Guiting Houa,⇑, K.R. Harib, Wulin Shua
M = 7 were recorded in the Longmenshan thrust system over the last millennium (Tang and Han, 1993; Division of Earthquake Mon-itoring and Prediction, China Seismologic Bureau, 1995, 1999).
The broader study, of which this is a part, entails a multidisci-plinary paleomagnetic, 40Ar/39Ar and U–Pb isotopic-dating, bio-stratigraphic, and chemostratigraphic study of PT boundary

Journal of Asian Earth Sciences sinoprobe.org

Circulation and oxygenation of the glacial South China Sea Dawei Lia, Tzu-Ling Chiangb, Shuh-Ji Kaoa,⇑, Yi-Chia Hsinc, Li-Wei Zhenga, Jin-Yu Terence Yanga,
A review of fossil rhinoceroses from the Neogene of Myanmar with description of new specimens from the Irrawaddy Sediments Zin-Maung-Maung-Theina,d,*, Masanaru Takaia, Takehisa Tsubamotob, Naoko Egia, Thaung-Htikec,
example, most research has focused on the eastern and southern YangtzeCraton, neglectingthe widespreadgranitoidsof the middle Yangtze Craton (MYC, Fig. 1A).
migmatite formation would allow to reconstruct the thermal evo-lution of the upper plate and then to discuss its geodynamic evolu-tion in the framework of the Himalaya–Tibet tectonic, petrologic
discontinuity within the sedimentary series of the Eastern Zone. One of the main structural features is the northwestward progres-sive weakening, and even disappearance of the cleavage plane.
96 F. Chirouze et al./Journal of Asian Earth Sciences 44 (2012) 94–106 Formation and from the middle to the upper Siwalik Formation was more or less coeval with the transitions observed in western

Journal of Asian Earth Sciences University of Southern


Journal of Asian Earth Sciences Sinica



The Asian monsoon system is an integral part of the global climatic system, and a deeper knowledge of it will contribute to a better un- derstanding of global atmospheric circulation and climate
Along the ductile detachment normal fault, several samples were collected in order to constrain the time of exhumation of the south-Liaodong peninsula MCC using the laser probe single
Journal of Asian Earth Sciences has an open access mirror journal Journal of Asian Earth Sciences: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review. The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to …
foraminiferal limestone in the latest Permian (Changhsingian) which then succeeds upwards into the Triassic. Permian–Triassic sediments of both terranes are often volcaniclastic and tuffaceous.

Journal of Asian Earth Sciences University of Malaya


Journal of Asian Earth Sciences colorado.edu

deposit within the Tethyan Himalaya, except for the shaley Kong Formation that lies immediately under the Spontang Ophiolite. The Stumpata Quartzite is a massive, thick-bedded texturally and
2.1.1. Dacite Porphyritic dacite is widespread across the northern and east-ern parts of Ataúro, where it most commonly occurs as an in situ hyaloclastite breccia of angular to sub-angular clasts up to 50 cm
localities, a Late Miocene-Pliocene activation was proposed based on chronologic data (Catlos et al., 2004; Harrison et al., 1997). In addition, brittle deformation has also been commonly identified
Preface Introduction to special issue: Geology of the Lake Baikal region The region around Lake Baikal (Fig. 1) is an outstanding natural laboratory for studying geological processes of the Earth’s crust
using a JSM-5600 scanning electron microscope in the State Key Laboratory of Solid Lubrication, Lanzhou Institute of Chemical Physics, Chinese Academy of Sciences, Lanzhou, China.
gases from Liaodong area are N 2-dominant, and contain low CO 2 and CH 4 from 0.1% to 2% and from 0.004% to 0.7%, respectively. d13C values of CO 2 vary greatly from 13‰ to 32‰, indicating
We restudied the Tamayen HP–LT occurrence by investigating the field relationships, petrographic characteristcs, mineral compositions, and P–T implications.
granite was found in this study. The difference between the Jerai granite and the other Main Range granite is the presence of peg-matites (associated with aplites), which cut the granite and sur-
The Cenozoic on-shore basins of Northern Vietnam: Biostratigraphy, vertebrate and invertebrate faunas Madelaine Böhmea,⇑, Jérôme Prietoa,b, Simon Schneiderc, Nguyen Viet Hungd, Do Duc Quangd,

Journal of Asian Earth Sciences University of Tokyo

Review Ophiolites of Iran: Keys to understanding the tectonic evolution of SW Asia: (II) Mesozoic ophiolites Hadi Shafaii Moghadama,⇑, Robert J. Sternb
thickness (from meters to centimeters) and sharp boundaries (Fig. 2b–d). Pyroxenes vary in abundance on various scales, and thus the lithology could be termed as either garnet lherzolite or
H.-L. Wang et al./Journal of Asian Earth Sciences 37 (2010) 286–291 287. 3. Methodology The crustal thickness at each station was estimated from the Moho P-to-S converted phase and its later crustal multiples shown on the radial receiver functions. In order to remove the source and instrument effects, receiver functions were obtained by using a time-domain iterative deconvolution technique
sequence of aftershocks (Kisslinger and Jones, 1991; Utsu et al., 1995; Wiemer and Katsumata, 1999). Assuming that the magnitude and occurrence time of earth-
a Department of Earth, Ocean and Atmospheric Science, Florida State University and National High Magnetic Field Laboratory, Tallahassee, FL 32306-4100, USA b Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China
Journal of Earth Science (previously known as Journal of China University of Geosciences), issued bimonthly through China University of Geosciences, covers all branches of geology and related technology in the exploration and utilization of earth resources.
a Department of Geology, Faculty of Science, The Maharaja Sayajirao University of Baroda, Vadodara 390002, India b CSIR Fourth Paradigm Institute (Formerly CSIR Centre for Mathematical Modeling and Computer Simulation (C-MMACS)), NAL Belur Campus, Bengaluru 560 037,
Geochemical study of the Cambrian–Ordovician meta-sedimentary rocks from the northern Altai-Mongolian terrane, northwestern Central Asian Orogenic Belt: Implications on …


Taknar Fault. Along the still recently active sinistral strike-slip fault of the Great Kavir system the Taknar uplift is in direct contact with
The Deccan tholeiite lavas and dykes of Ghatkopar–Powai area, Mumbai, Panvel flexure zone: Geochemistry, stratigraphic status, and tectonic
First Triassic palaeomagnetic constraints from Junggar (NW China) and their implications for the Mesozoic tectonics in Central Asia Flavien Chouleta,⇑, Yan …

Robert Hall Google Scholar Citations

Journal of Earth Science springer.com

Journal of Asian Earth Sciences cugb.edu.cn


JOURNAL OF ASIAN EARTH SCIENCES Elsevier

Journal of Asian Earth Sciences Sorbonne Université

Journal of Asian Earth Sciences colorado.edu
Journal of Asian Earth Sciences WordPress.com

Shallow crustal and intermediate-depth events with 4.0 > M P 2.0 that occurred between February and July, 2006, recorded at 189 Hi-net seismic stations in SW Japan have been
thickness (from meters to centimeters) and sharp boundaries (Fig. 2b–d). Pyroxenes vary in abundance on various scales, and thus the lithology could be termed as either garnet lherzolite or
The Deccan tholeiite lavas and dykes of Ghatkopar–Powai area, Mumbai, Panvel flexure zone: Geochemistry, stratigraphic status, and tectonic
Moyra E.J. Wilson Senior Lecturer, Earth Sciences, University of Western Australia (UWA), Perth, Australia Verified email at uwa.edu.au Chris Morley Petroleum Geophysics MSc Program, Chiang Mai University, Chiang Mai, Thailand
The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology , tectonics , geochemistry and geophysics of Asia.
Taknar Fault. Along the still recently active sinistral strike-slip fault of the Great Kavir system the Taknar uplift is in direct contact with
Geochemical and isotopic constraints on the evolution of Late Paleozoic dyke swarms in West Junggar, Xinjiang, China Yan Zhana, Guiting Houa,⇑, K.R. Harib, Wulin Shua

Journal of Asian Earth Sciences USGS
Journal of Asian Earth Sciences geol.lsu.edu

Journal of Asian Earth Sciences Review Articles Recently published review articles from Journal of Asian Earth Sciences Review Articles The Sipoholon Geothermal Field and adjacent geothermal systems along the North-Central Sumatra Fault Belt, Indonesia: Reviews on geochemistry, tectonics, and natural heat loss
Molchan and Kagan, 1992), which motivates us to carry out the statistical analysis examining the SIPs of GPS TEC in China. In this study, GIM TECs are investigated for 56 M P 6.0 earth-
The shear-wave splitting in the crust and the upper mantle around the Bohai Sea, North China Shi Yutao⇑, Gao Yuan, Tai Lingxue, Fu Yuanyuan Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, PR China
Geochemical and isotopic constraints on the evolution of Late Paleozoic dyke swarms in West Junggar, Xinjiang, China Yan Zhana, Guiting Houa,⇑, K.R. Harib, Wulin Shua
Moyra E.J. Wilson Senior Lecturer, Earth Sciences, University of Western Australia (UWA), Perth, Australia Verified email at uwa.edu.au Chris Morley Petroleum Geophysics MSc Program, Chiang Mai University, Chiang Mai, Thailand
The Asian monsoon system is an integral part of the global climatic system, and a deeper knowledge of it will contribute to a better un- derstanding of global atmospheric circulation and climate
deposit within the Tethyan Himalaya, except for the shaley Kong Formation that lies immediately under the Spontang Ophiolite. The Stumpata Quartzite is a massive, thick-bedded texturally and
terrains of the Indus River system when a given river drains only a single source terrain. This technique was used to constrain the source of the sediment in the modern stream and to compare this

Journal of Asian Earth Sciences jaeger.earthsci.unimelb
Journal of Asian Earth Sciences sourcedb.igg.cas.cn

The shear-wave splitting in the crust and the upper mantle around the Bohai Sea, North China Shi Yutao⇑, Gao Yuan, Tai Lingxue, Fu Yuanyuan Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, PR China
sequence of aftershocks (Kisslinger and Jones, 1991; Utsu et al., 1995; Wiemer and Katsumata, 1999). Assuming that the magnitude and occurrence time of earth-
a Department of Earth, Ocean and Atmospheric Science, Florida State University and National High Magnetic Field Laboratory, Tallahassee, FL 32306-4100, USA b Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China
Differential destruction of the North China Craton: A tectonic perspective Yan-Jie Tanga,⇑, Hong-Fu Zhanga,b, M. Santoshc, Ji-Feng Yinga a State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China
thickness (from meters to centimeters) and sharp boundaries (Fig. 2b–d). Pyroxenes vary in abundance on various scales, and thus the lithology could be termed as either garnet lherzolite or
surface or the axial plane cleavage varies within the domain, and is consistent with the sinuous hinge lines on the geologic map. At the outcrop level, variation in the dip angle of fold hinge lines is com-
A review of fossil rhinoceroses from the Neogene of Myanmar with description of new specimens from the Irrawaddy Sediments Zin-Maung-Maung-Theina,d,*, Masanaru Takaia, Takehisa Tsubamotob, Naoko Egia, Thaung-Htikec,
The Deccan tholeiite lavas and dykes of Ghatkopar–Powai area, Mumbai, Panvel flexure zone: Geochemistry, stratigraphic status, and tectonic
2. Geological setting and petrography The jadeite uplift (Fig. 1) containing the Myanmar jadeite deposit and high-pressure rocks in Hpakan area of Kachin State
Tsunami hazard from the subduction megathrust of the South China Sea: Part I. Source characterization and the resulting tsunami Kusnowidjaja Megawatia,b,*, Felicia …
helping to create an assessment of the geothermal potential for electric generation from the Hammam Faraun hot spring. Previous studies have been conducted on the geological and
H.-L. Wang et al./Journal of Asian Earth Sciences 37 (2010) 286–291 287. 3. Methodology The crustal thickness at each station was estimated from the Moho P-to-S converted phase and its later crustal multiples shown on the radial receiver functions. In order to remove the source and instrument effects, receiver functions were obtained by using a time-domain iterative deconvolution technique
effort has been devoted to estimate differences between SH-wave velocity and SV-wave velocity both regionally (Villasenˇor et al., 2001) and globally (Shapiro and Ritzwoller, 2002).