2005•Tianranqi diqiu kexueRequires access

THE TECTONIC CHARACTERISTICS OF YINGJISU DEPRESSION IN TARIM BASIN

Liu Yu-kui

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Abstract

Yingjisu depression lies in north of the Tarim basin as same as Kuche depression,they have the same deposit-tectonic evolution history. Yingjisu depression is separated Two hollows and one according to exploration and Mesozoic tectonic-structure, they are Yingxi hollow, Weimake-alagan low protruding and Yingdong hollow,it is separated five triple-tectonic parts particularly. Many northwestern and northeastern reverse-fauts lie in the region.It is a slide-extruding basin for the Aljin mountain moving,and emerged a mode of broad-slow Bullhead in the seismic sections.

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What this paper is about

Yingjisu depression lies in north of the Tarim basin as same as Kuche depression,they have the same deposit-tectonic evolution history. Yingjisu depression is separated Two hollows and one according to exploration and Mesozoic tectonic-structure, they are Yingxi hollow, Weimake-alagan low protruding and Yingdong hollow,it is separated five triple-tectonic parts particularly. Many northwestern and northeastern reverse-fauts lie in the region.It is a slide-extruding basin for the Aljin mountain moving,and emerged a mode of broad-slow Bullhead in the seismic sections.

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Available abstract

Yingjisu depression lies in north of the Tarim basin as same as Kuche depression,they have the same deposit-tectonic evolution history. Yingjisu depression is separated Two hollows and one according to exploration and Mesozoic tectonic-structure, they are Yingxi hollow, Weimake-alagan low protruding and Yingdong hollow,it is separated five triple-tectonic parts particularly. Many northwestern and northeastern reverse-fauts lie in the region.It is a slide-extruding basin for the Aljin mountain moving,and emerged a mode of broad-slow Bullhead in the seismic sections.

Key concepts: Geology, Tectonics, Structural basin, Tarim basin, Mesozoic, Paleontology, Depression (economics), Geomorphology

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