摘要
本文以三工河为例,将该区划分为高台地冰期(Q<sub>p1</sub>)、洼地冰期(Q<sub>p2</sub>),天池冰期(Q<sub>p3</sub><sup>1</sup>)和力行达坂冰期（Q（<sub>p</sub>3）<sup>3</sup>）。对该区新构运动的性质、类型、特点作了较详细的阐述,并指出新构造运动的间歇期和波动期及其与冰期和间冰期的对应关系。最后运用深部地质资料揭示出博格达山新构造运动的源动力。
In the paper Sangonghe is taken as an example to subdivide the Quaternary glacier of the study area into four glacial stage, i.e., Gaotaidi glacial stage (QP1). Wadi glacial stage ( QP2 ), Tianchi glacial stage ( QP3 ) and Lixingdaban glacial stage ( Qp33 ) .
The characteristics and types of the neotectonic movement are described in detail as well as the intermittent period and undulate period which correspond irrespectively to the glacial stage and interglacial stage. The source power of the neotectonic movement in Bogda mountain is also revealed by data from the deep
earth.
出处
《新疆地质》
CAS
CSCD
1992年第1期40-50,共11页
Xinjiang Geology
关键词
博格达山
第四纪古冰川
新构造运动
Bogda mountain, Quaternary paleoglacier, nrotectonic movement
