Results 231 to 240 of about 1,874 (245)
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The Palaeo-Tethyan Realm and Indosinian Orogenic System of Southeast Asia

1989
Southeast Asia is a composite of relatively stable blocks of Precambrian continental crust overlain in large part by Palaeozoic carbonate-dominated platforms. The blocks are sutured along highly deformed mobile belts characterized by deep water sediments and fragmented ophiolites.
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Determination of Onset of Uplifting for the Mid‐Upper Yangtze Area Since Indosinian Event

Chinese Journal of Geophysics, 2010
AbstractThe onset of uplifting of the Mid‐upper Yangtze area is constrained by the combination of analysis of apatite fission track (AFT) age and modeling of fission track length distribution. The results show that the general trend of onset of uplifting is characterized by decreasing westward in geological time for the different tectonic units in the ...
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Discovery of the Indosinian aluminum A-type granite in Zhejiang Province and its geological significance

Science China Earth Sciences, 2012
Zircon LA-ICP-MS U-Pb dating of the Jingju syenogranites in the southwestern part of Zhejiang Province shows that these rocks were crystallized in the Late Triassic at 215±2 Ma, rather than in the Cretaceous as previously proposed. The Jingju syenogranites are characterized by relatively high K2O and FeO*, and low MgO.
WanYou Li   +3 more
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Unconformity of red sandstones in north Vietnam: field evidence for Indosinian orogeny in northern Indochina?

Terra Nova, 1998
We re‐examine several unconformity sites in northwestern Vietnam where the Indosinian orogenesis has been defined. Field observations in the Black‐River (Song Da) region, near Son La, demonstrate that red sandtones and conglomerates, reportedly of Cretaceous age, occur unconformably above schistosed epimetamorphic middle‐Triassic sediments.
null Lacassin   +3 more
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Tectonics of Late Permian-Triassic (The Indosinian Tectonic Period, 260–200 Ma)

2010
Major collision and amalgamation of continental fragments occurred in the Chinese continent during the Indosinian Tectonic Event; the Lancangjiang (i.e. Lazhulung-Shuanghu-Changning-Menglian-Dak of Thailand-central Malaya Peninsula, 1 in Fig. 6.3), Jinshajiang (18 in Fig. 6.3), Qinling-Dabie (6,10 and 11 in Fig.
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Metallogenic Response of Ailaoshan Gold Belt in Indosinian Orogeny

Acta Geologica Sinica - English Edition, 2014
Guiyong SHI   +4 more
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Indosinian tectonics and mineral systems in China: an introduction

Geological Journal, 2014
Yan‐Jing Chen   +3 more
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The Indosinian orogeny is South-East Asia

2017
Golonka Jan   +4 more
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