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By Marc S. Hendrix, Gregory Arlen Davis

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Extra resources for Paleozoic and Mesozoic tectonic evolution of central Asia: from continental assembly to intracontinental deformation, Nummer 194

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213–231. , 1985, The Precambrian of Tianshan, Xinjiang: Xinjiang Geology, v. 3, p. 14–25. , 1985a, The Sinian in AksuWushi Region, Xinjiang, China: Urumqi, Xinjiang People’s Publishing House, 184 p. , 1985b, The Sinian in Xinjiang: Urumqi, China, Xinjiang People’s Publishing House, 173 p. , 1975, Himalayan-Bengal model for flysch dispersal in the Appalachian-Ouachita system: Geological Society of America Bulletin, v. 86, p. 273–286. , 1990, Characteristics of selected petroleum source rocks, Xinjiang Uygur Autonomous Region, northwest China: American Association of Petroleum Geologists Bulletin, v.

445–456. , 1997, Tectonic controls on facies transitions in an oblique collision: The western Soloman Sea, Papua New Guinea: Geological Society of America Bulletin, v. 109, p. 1266–1278. D. thesis]: Beijing, Chinese Academy of Geological Sciences, 90 p. , 1994, New observation of the Upper Silurian Akeyazi and Qiongkushitai formations on the northern slope of the Halik mountains: Regional Geology of China, v. 1994, p. 240–245. , 1995, The mineralogy, petrology, metamorphic PTDt trajectory and exhumation mechanism of blueschists, south Tian Shan, northwestern China: Tectonophysics, v.

And is not yet complete. Applying these observations to the late Paleozoic Tian Shan, we envision an initial encounter between Tarim and the central Tian Shan occurring near the Devonian-Carboniferous boundary (perhaps reflected in the Devonian-Carboniferous unconformity observed in northern Tarim and the central Tian Shan), with subsequent rotational closure of the south Tian Shan remnant ocean basin throughout the Early Carboniferous accounting for blueschist-metamorphic and arc-igneous radiometric ages in the paired belts of the southern central Tian Shan (Fig.

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