| 博格达山北坡第四纪古冰川与新构造运动 |
| |
| 引用本文： | 朱毅莹,赵剑峰.博格达山北坡第四纪古冰川与新构造运动[J].新疆地质,1992(1). |
| |
| 作者姓名： | 朱毅莹 赵剑峰 |
| |
| 作者单位： | 新疆工学院
(朱毅莹)，新疆工学院(赵剑峰) |
| |
| 摘 要： | 本文以三工河为例,将该区划分为高台地冰期(Q_(p1))、洼地冰期(Q_(p2)),天池冰期(Q_(p3)~1)和力行达坂冰期(Q(_p3)~3)。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。
|
| 关 键 词： | 博格达山 第四纪古冰川 新构造运动 |
QUATERNARY PALEOGLACIER AND NEOTECTONIC MOVEMENT ON THE NORTHERN SLOPE OF BOGDA MOUNTAIN |
| |
| Zhu Yiying Zhao Jianfeng.QUATERNARY PALEOGLACIER AND NEOTECTONIC MOVEMENT ON THE NORTHERN SLOPE OF BOGDA MOUNTAIN[J].Xinjiang Geology,1992(1). |
| |
| Authors: | Zhu Yiying Zhao Jianfeng |
| |
| Institution: | Xinjiang College of Engineering and Technology |
| |
| Abstract: | 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. |
| |
| Keywords: | Bogda mountain Quaternary paleoglacier nrotectonic movement |
| 本文献已被 CNKI 等数据库收录！ |
