|
|||||
|
|
| 塔里木板块早—中二叠世玄武质岩浆作用的沉积响应 | |
| 引用本文： | 陈汉林 杨树锋 王清华,罗俊成 贾承造 魏国齐 厉子龙 何光玉 胡安平.塔里木板块早—中二叠世玄武质岩浆作用的沉积响应[J].中国地质,2006,33(3):545-552. |
| 作者姓名： | 陈汉林 杨树锋 王清华 罗俊成 贾承造 魏国齐 厉子龙 何光玉 胡安平 |
| 作者单位： | 1. 浙江大学理学院地球科学系,浙江,杭州,310027 2. 浙江大学理学院地球科学系,浙江,杭州,310027;中国石油天然气股份有限公司塔里木油田分公司,新疆,库尔勒,841000 3. 中国石油天然气股份有限公司塔里木油田分公司,新疆,库尔勒,841000 4. 中国石油勘探开发研究院,北京,100087 |
| 基金项目： | 国家高技术研究发展计划(863计划);国家研究发展基金 |
| 摘 要： | 塔里木板块内部发育了大量由早—中二叠世板内岩浆作用所形成的、以玄武岩类为主的基性岩浆岩,包括玄武岩、辉绿岩、玄武安山岩等,残余分布面积约20万km2。而二叠纪时期是塔里木板块演化过程中一个非常重要的转折时期,从早二叠世晚期开始塔里木板块结束了海相沉积,进入了陆相沉积阶段。通过对塔里木板块的岩浆作用特征和石炭纪—二叠纪沉积相的分析,笔者讨论了这一大规模的岩浆作用对板块晚石炭世—二叠纪的沉积作用所起的控制作用,提出了塔里木板块早—中二叠世巨量玄武质岩浆作用的沉积响应过程模式。 |
| 关 键 词： | 塔里木板块 早—中二叠世 玄武质岩浆作用 沉积作用 沉积响应模式 |
| 文章编号： | 1000-3657（2006）03-0545-08 |
| 收稿时间： | 2006-05-10 |
| 修稿时间： | 2006-05-102006-05-27 |
Sedimentary response to the Early-Mid Permian basaltic magmatism in the Tarim plate |
|
| CHEN Han-lin,YANG Shu-feng,WANG Qing-hu,LUO Jun-cheng,JIA Cheng-zao,WEI Guo-qi,LI Zi-long,HE Guang-yu,HU An-ping.Sedimentary response to the Early-Mid Permian basaltic magmatism in the Tarim plate[J].Chinese Geology,2006,33(3):545-552. | |
| Authors: | CHEN Han-lin YANG Shu-feng WANG Qing-hu LUO Jun-cheng JIA Cheng-zao WEI Guo-qi LI Zi-long HE Guang-yu HU An-ping |
| Institution: | 1. Department of Earth Sciences, Zhejiang University, Hangzhou 310027, Zhejiang, China; 2. Tarim Oil Field Branch, PetroChina, Korla 841000, Xinjiang , China; 3. Institute of Petroleum Exploration and Development, PetroChina, Beijing 100087, China |
| Abstract: | In the Tarim plate there is a great deal of basic igneous rocks including basalt,diabase and basaltic andesite formed by the Early to Middle Permian intraplate magmatism,and their residuals cover an area of about 200 000 km2.The Permian was a very important transition stage in the evolution of the Tarim plate.In the late Early Permian the Tarim basin ended marine sedimentation and entered the stage of continental sedimentation.On the basis of an analysis of the characteristic of the Early to Middle Permian basaltic magmatism and Carboniferous to Permian sedimentary facies in the Tarim basin,this paper discusses the controls of this large-scale magmatism on the Carboniferous to Permian sedimentation and puts forward a model of the sedimentary response to the Early to Middle Permian basaltic magmatism in the Tarim plate. |
| Keywords: | Tarim plate Early to Middle Permian basaltic magmatism sedimentation sedimentary response model |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ | |
| 点击此处可从《中国地质》浏览原始摘要信息 | |
| 点击此处可从《中国地质》下载免费的PDF全文 | |