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Tectonics of Late Permian-Triassic (The Indosinian Tectonic Period, 260–200 Ma)
2010Major 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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59th U.S. Rock Mechanics/Geomechanics Symposium
ABSTRACT: Granite is a product of crustal melting and intrusion cooling at depths of 10-15km and deeper underground, representing a tectonic environment under certain temperature and pressure conditions. It was exposed to the surface through tectonic uplift and erosion and underwent weathering and alteration.
Jianyun Feng +6 more
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ABSTRACT: Granite is a product of crustal melting and intrusion cooling at depths of 10-15km and deeper underground, representing a tectonic environment under certain temperature and pressure conditions. It was exposed to the surface through tectonic uplift and erosion and underwent weathering and alteration.
Jianyun Feng +6 more
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Indosinian tectonics and mineral systems in China: an introduction
Geological Journal, 2014Yan‐Jing Chen +3 more
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Metallogenic Response of Ailaoshan Gold Belt in Indosinian Orogeny
Acta Geologica Sinica - English Edition, 2014Guiyong SHI +4 more
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Indosinian Tectogeny in the geological correlation of Vietnam and adjacent regions
1997J. M. Dickins, Phan Cu Tien
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Indosinian orogenic belt: Song Chay tectonic belt
Acta Petrologica SinicaWei LIN +6 more
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