UPLIFTING PROCESS OF EASTERN TIANSHAN MOUNTAINS: EVIDENCE FROM FISSION-TRACK AGE AND ITS TECTONIC SIGNIFICANCE
UPLIFTING PROCESS OF EASTERN TIANSHAN MOUNTAINS: EVIDENCE FROM FISSION-TRACK AGE AND ITS TECTONIC SIGNIFICANCE
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发表时间：
2002
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影响因子：
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通讯作者：
Fang Shi-hu
中科院分区：
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作者：
Fang Shi-hu
The uplift of the basement in the eastern Tianshan mountains was mainly completed during the Cretaceous, after which no rapid uplift occurred. The present tectonic framework of the eastern Tianshan mountains basically inherits that of the Mesozoic, but that of the western Tianshan mountains was mainly formed during the Cenozoic intracontinental orogeny. The difference is caused by scissor-like closure of the southern Tianshan oceanic basin starting from west to east and oblique collision of Tarim block with terranes lying toward north during the late Paleozoic.
