ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西天山中新生代古高程恢复研究
  
关键词:oxygen isotope  vesicular-basalt  apatite fission track  pebble components  paleoelevation  Mesozoic–Cenozoic  Western Tianshan
基金项目:国家自然科学基金新疆联合重点基金项目(编号: U1403292); 国家科技支撑计划项目(编号: 2015BAB05B04); 中国地质调查局地质调查工作项目(编号: DD2016053)
作者单位E-mail
张文高 中国地质科学院地质力学研究所 547027367@qq.com 
陈正乐 中国地质科学院地质力学研究所 chenzhengle@263.com 
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摘要:
Study on the Reconstruction of Mesozoic–Cenozoic Paleoelevation in the Western Tianshan
      The Tianshan mountain is located in the middle part of the Central Asian orogenic belt, stretching for nearly 2 500 km from the east to the west as a whole. The formation of the modern Tianshan is not only directly related to the plate subduction and collision orogenesis in Paleozoic, but also influenced by the far-distance effect of Indian-Asian collision in Ceno-zoic. The Cenozoic uplift and exhumation history of the Tianshan Mountain can help us to study the kine-matic and dynamic processes of orogenic belt inside Asian continent. In order to better understand how and when the topography of modern Tianshan was build, this study on reconstruction of paleoelevation in Sikeshu drainage basin, Tuoyun basin, north and mid-dle part of west Tianshan. In addition, from the study of structure deformation and sedimentation in fore-land basin, we discuss the the history of the Meso-zoic-Cenozoic paleoelevation in different parts of west Tianshan mountion.
ZHANG Wen-gao,CHEN Zheng-le.2017.Study on the Reconstruction of Mesozoic–Cenozoic Paleoelevation in the Western Tianshan[J].Acta Geoscientica Sinica,38(s1):69-72.
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