金沙江中游云南龙街粉砂层沉积环境演化特征  

Sedimentary environment evolutionary characteristics of Longjie silt layer in the middle reaches of the Jinsha River,Yunnan

作　　者：李朝柱[1,2] 王书兵[1,2] 傅建利[1,2] 蒋复初[1,2,3] 

机构地区：[1]中国地质科学院地质力学研究所,北京100081 [2]国土资源部新构造运动与地质灾害重点实验室,北京100081 [3]中国科学院湖泊沉积与环境开放研究实验室,江苏南京210008

出　　处：《地质通报》2015年第1期113-120,共8页Geological Bulletin of China

基　　金：国家自然科学基金项目(批准号:40772211);中国科学院湖泊沉积与环境开放研究实验室基金项目(编号:HB0304)

摘　　要：沿金沙江攀枝花三堆子至武定县白马口段河谷两岸分布一套以灰黑色、灰黄色、灰白色粉砂、粘土质粉砂和粘土为主的湖相地层，尤以云南省元谋县龙街盆地内最为发育，被称为龙街粉砂层。通过龙街YA钻孔和龙街、白泥湾剖面的磁性地层学和光释光年代学的研究，探讨龙街粉砂层的时代与归属。龙街YA钻孔地层厚度101.18m，其中龙街粉砂层厚92.96m，上覆7.5m的红棕色细砂和砂砾石层，下伏厚度大于0.72m的灰绿色含角砾粗砂。综合分析YA钻孔的磁性地层学和光释光年龄，认为获取龙街粉砂层的沉积时代为150~30ka BP，属于晚更新世。通过地层沉积特征变化，反演晚更新世以来湖泊的形成及沉积环境变化，探讨晚更新世以来区域新构造的活动阶段及其对河流演化过程的控制作用。The Longjie silt layer consists of a series of silt, silty clay and clay lacustrine sediments which are grayish black, grayish yel？low and grayish white in color. This silt layer is distributed along the valley of the Jinsha River from Sanduizi of Panzhihua City to Baimakou of Wuding County, and is well developed in the Longjie basin in Yunnan Province. The Longjie drill hole intersects the stratatigraphic thickness of 101.18m, which includes 92.96m Longjie silt layer. Its sedimentation occurred about 150~30ka BP, as shown by the analysis of magnetostratigraphy and OSL dating. Through the study of sedimentary variation characteristics, this paper deals with the formation process of Longjie silt layer, the relative regional neotectonics movement stage and its influence on the devel？opment of the Jinsha River.

关 键 词：金沙江 龙街粉砂层 上更新统 新构造 

分 类 号：P534.631[天文地球—第四纪地质学]