Zobrazeno 1 - 10
of 50
pro vyhledávání: '"Ching-Ying Lan"'
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 19, Iss 3, p 257 (2008)
We present a new synthesis of the tectono-thermal events of Taiwan, excluding the Coastal Range, based on existing isotopic, geochemical and geochronological data for granitic, metamorphic, volcanic and sedimentary rocks. Nd model ages (TDM) and the
Externí odkaz:
https://doaj.org/article/f5e3605bcd344cf7b63da08dc7335f49
Publikováno v:
International Geology Review. 59:333-346
Various tectonic models have been proposed to account for the widely distributed igneous activities in the southeastern part of the South China Block (SCB) during the Triassic–Jurassic period. One of the major contending debates is on the timing of
Autor:
Thi Dung Pham, J. Gregory Shellnutt, Trong-Hoa Tran, Andrey E. Izokh, Alexander S. Borisenko, Tuan Anh Tran, Ngoc Can Pham, Ching Ying Lan, Thi Phuong Ngo, Tadashi Usuki
Publikováno v:
Journal of Asian Earth Sciences. 109:1-19
Major and trace elements and whole rock Sr–Nd isotope data of Late Permian silicic plutonic and volcanic rocks from the Phan Si Pan–Tu Le region in NW Vietnam were collected in order to establish their petrogenetic relationship with the magmatic
Autor:
Kuo-Lung Wang, Ching Ying Lan, Sun-Lin Chung, Tadashi Usuki, Trong-Hoa Tran, Gregory Shellnutt, Thi Dung Pham
Publikováno v:
Journal of Asian Earth Sciences. 97:102-124
In-situ zircon U–Pb and Hf isotope analyses were carried out for alkaline silicic magmatic rocks from the Phan Si Pan-Tu Le region in northern Vietnam to constrain their possible sources and to determine their petrogenetic relationship with the Eme
Autor:
Huai Jen Yang, Ching Ying Lan, Kuo-Lung Wang, Wen Yu Hsu, Trinh Van Long, Tadashi Usuki, J. Gregory Shellnutt, Y. Iizuka, Sun-Lin Chung, Stanley A. Mertzman
Publikováno v:
Lithos. :229-241
Cordilleran-type batholiths are useful in understanding the duration, cyclicity and tectonic evolution of continental margins. The Dalat zone of southern Vietnam preserves evidence of Late Mesozoic convergent zone magmatism superimposed on Precambria
Publikováno v:
Tectonophysics. 586:145-159
To constrain the paleoposition of Indochina within Gondwana during the Early Paleozoic, we performed in-situ U–Pb and Hf isotope analyses on detrital zircons from three river sediment samples in the Truong Son Belt of the Indochina block. The age d
Autor:
Bor-ming Jahn, Takaomi Yokoyama, Kenshi Maki, Hao-Tsu Chu, Ching Ying Lan, Yoshiaki Kon, Takafumi Hirata, W. G. Ernst, Tzen-Fu Yui
Publikováno v:
Tectonophysics. :31-42
Taiwan formed during the Plio-Pleistocene collision of Eurasia with the outboard Luzon arc. Its pre-Tertiary basement, the Tananao metamorphic complex, consists of the western Tailuko belt and the eastern Yuli belt. These circum-Pacific belts have be
Autor:
Kenshi Maki, Yoshiyuki Iizuka, Tadashi Usuki, Ching Ying Lan, Chao Ming Wu, Tzen-Fu Yui, Marty Grove, Kuo-Lung Wang, Uwe Martens, Tsai Way Wu, Juhn G. Liou, Tadao Nishiyama
Publikováno v:
European Journal of Mineralogy. 24:263-275
Zircon separates from one jadeitite sample (JJ) from Tone, Japan and one from Guatemala (GJ) were studied for mineral inclusions, age dating, trace-element determination and Hf isotope analysis. These zircons can be categorized into two types. Type I
Autor:
Tran Ngoc Nam, Ching-Hua Lo, Pei-Ling Wang, Sun-Lin Chung, Yuji Sano, Ching Ying Lan, Tung Yi Lee
Publikováno v:
Journal of Asian Earth Sciences. 40:1044-1055
The PoSen complex, located closely adjacent to the southwestern margin of the Red River shear zone represents the uplifted basement of north Vietnam and may record the motion of the shear zone. However, its thermochronological history has not been fu
Autor:
Tzen-Fu Yui, Kenshi Maki, Uwe Martens, Tsai-Way Wu, Tadashi Usuki, Chao-Ming Wu, Juhn G. Liou, Ching Ying Lan
Publikováno v:
Chemical Geology. 270:45-55
Zircons from one jadeitite sample, collected from serpentinite melange north of the Motagua fault, Guatemala, were separated for SHRIMP-RG U–Pb dating and trace element analyses. The sub- to anhedral crystal form, lack of typical magmatic oscillato