新疆艾比湖东南缘K3孔晚新生代环境演化

现代地质 ›› 2009, Vol. 23 ›› Issue (6): 1012-1021.

新疆艾比湖东南缘K3孔晚新生代环境演化

张金起¹, 刘斌^2,3, 陈旭光⁴, 孙晓明¹, 王云生⁵

1中国地质调查局天津地质矿产研究所，天津300170；2中国地质大学地球科学与资源学院，北京100083；
3新疆地质矿产局，新疆乌鲁木齐830000；4新疆地质勘查局第二水文地质大队，新疆昌吉831100；
5中钢集团天津地质研究院，天津300061

收稿日期:2009-03-23 修回日期:2009-09-20 出版日期:2009-12-29 发布日期:2012-02-16
作者简介:张金起，男，工程师，1954年出生，磁性地层与晚新生代地质专业，主要从事第四纪地质及磁性地层的研究工作。Email:tjzjq@sina.com。

Environmental Evolution at the Drilling Hole K3 in the East-south Margin of Ebinur Lake, Xinjiang in Late Cenozoic

ZHANG Jin-Qi¹, Liu-Bin^2,3, Chen Xu-Guang⁴, Sun Xiao-Ming¹, Wang Yun-Sheng⁵

1Tianjin Institute of Geology and Mineral Resources, China Geological Survey, Tianjin300170, China；2School of the Earth Sciences and
Resources，China University of Geosciences, Beijing100083, China；3Xinjiang Geological Mineral Resources Bureau, Urumqi，Xinjiang830000,
China；4The 2nd Hydrology and Geological Team, Xinjiang Geological Investigation Bureau, Changji，Xinjiang831100, China；
5Tianjin Geological Institute, Sinosteel Corporation, Tianjin300061, China

Received:2009-03-23 Revised:2009-09-20 Online:2009-12-29 Published:2012-02-16

摘要/Abstract

摘要：

新疆准格尔盆地艾比湖K3孔孔深500.8 m，岩心采取率80.4%。依据光释光(OSL)测年、磁性地层学、磁化率、微体古生物(介形类和有孔虫)、孢粉学和岩相学研究，确定了K3孔晚新生代以来的环境演化过程：该孔钻遇地层属于约4.2 Ma以来沉积，在约3.6～4.2 Ma时期此地是湖泊环境；大约自3.6 Ma以来，伴随着青藏高原快速隆升发生的哈密运动，该区沉积环境由半深湖和浅湖演变为滨湖和水下三角洲，研究区干旱化状况加剧；在约2.6～3.0 Ma的上新世末期，形成盆地边缘和冲积扇体系；2.6 Ma前后，在西域运动—盐水沟运动影响下，研究区是曲流河体系发育期；自“中更新革命”约0.8 Ma以来，全区干旱化状况与现代相近。4.2 Ma以来不连续的孢粉图示和介形类的分布，也显示了沉积动力和水体的复杂变化；构造-气候旋回控制了该地晚新生代环境演化。

关键词: 晚新生代, 构造-气候旋回, 环境演化, 新疆艾比湖

Abstract:

The 500.8 meters depth drilling hole K3 with a core recovery efficiency of 80.4% is located at the eastsouth margin of Ebinur Lake in Zhunger Basin, Xinjiang. Based on the study of OSL dating, palaeomagnetism, susceptibility, micropaleontology (ostracoda and foraminifera), palynology and lithostratigraphy in the borehole, it is determined that the drilled sequences belong to the deposits since cir. 4.2 Ma，there was a lake environment during 3.6-4.2 Ma ，and since cir. 3.6 Ma the sedimentary environment changed from hemi-deep or shallow lake to littoral lake or subaqueous delta accompanying with the Hami Movement as a result of the quickly uplifting of Qinghai-Tibet Plateau, the aridification situation was also aggravating in the study area; during Late Pliocene (cir. 2.6-3.0 Ma) there was a basin margin and fluvial fan sedimentary system; at cir. 2.6 Ma under the influence of the Xiyu Movement and Yanshuigou Movement, the meandering stream system was developed in the study area. Since the Middle Pleistocene Revolution i.e.cir. 0.8 Ma, the aridification situation was similar to that of modern times. The uncontinuous spore-pollen diagram and ostracoda distribution show a complicated development of sedimentary dynamics and water bodies since 4.2 Ma. The environmental change in the study area had been controlled by the tecto-climatic cycles.

Key words: Late Cenozoic, tecto-climatic cycle, environmental evolution, Ebinur Lake,Xinjiang

中图分类号:

P534.6

张金起, 刘斌, 陈旭光, 孙晓明, 王云生. 新疆艾比湖东南缘K3孔晚新生代环境演化[J]. 现代地质, 2009, 23(6): 1012-1021.

ZHANG Jin-Qi, Liu-Bin, Chen Xu-Guang, Sun Xiao-Ming, Wang Yun-Sheng. Environmental Evolution at the Drilling Hole K3 in the East-south Margin of Ebinur Lake, Xinjiang in Late Cenozoic[J]. Geoscience, 2009, 23(6): 1012-1021.

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