| 雪峰陆内多期复合造山带震旦—三叠纪沉积演化特征 |
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| 引用本文： | 李,聪 陈世悦 张鹏飞 杨怀宇 陈丽华.雪峰陆内多期复合造山带震旦—三叠纪沉积演化特征[J].中国地质,2011,38(1):43-51. |
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| 作者姓名： | 李 聪 陈世悦 张鹏飞 杨怀宇 陈丽华 |
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| 作者单位： | 1. 中国石油大学(华东)地球资源与信息学院,山东,青岛,266555
2. 中国石化胜利油田地质科学研究院,山东,东营,257015 |
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| 基金项目： | 中国石油化工股份有限公司项目(N0801058)资助 |
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| 摘 要： | 笔者通过对雪峰及其两侧震旦纪—三叠纪的地层沉积特征进行相关的野外调查和室内总结,基本明确了雪峰地区自震旦纪以来的隆凹变迁规律。根据雪峰地区的隆凹特征及古地理属性将雪峰地区震旦纪—三叠纪的构造沉积演化历程划分为五大阶段,分别为早震旦世—中奥陶世的斜坡-陆棚-盆地阶段;晚奥陶世—晚石炭世的隆起剥蚀阶段;二叠纪的碳酸盐岩台地阶段;早三叠世的碳酸盐质陆棚阶段和中三叠世—白垩纪的隆起—陆相山间盆地阶段。笔者从沉积角度证明雪峰的演化属性并非一个古陆区,而是一个多期复合叠加的陆内造山带。
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| 关 键 词： | 陆内造山带 雪峰隆起 沉积演化 |
Palaeozoic-Mesozoic sedimentary evolution characteristics of the Xuefeng Mountain intracontinental orogenic belt |
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| LI Cong,CHEN Shi-yue,ZHANG Peng-fei,YANG Huai-yu,CHEN Li-hua.Palaeozoic-Mesozoic sedimentary evolution characteristics of the Xuefeng Mountain intracontinental orogenic belt[J].Chinese Geology,2011,38(1):43-51. |
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| Authors: | LI Cong CHEN Shi-yue ZHANG Peng-fei YANG Huai-yu CHEN Li-hua |
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| Institution: | LI Cong1,CHEN Shi-yue1,ZHANG Peng-fei2,YANG Huai-yu2,CHEN Li-hua2(1.College of Geo-Resources and Information,CUP,Qingdao 266555,Shandong,China,2.Geological Science Research Institute of Shengli Oilfield Co.,Ltd.,SINOPEC,Dongying 257015,Shangdong,China) |
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| Abstract: | In this paper,the authors studied the characteristics of Palaeozoic-Mesozoic stratigraphic sedimentation in the Xuefeng Mountain and its lateral layers by means of field investigation and indoor analysis,and found out the regularity of uplifting-depression change in the Xuefeng Mountain since Palaeozoic.The course of tectono-sedimentary evolution from Palaeozoic to Mesozoic can be divided into five phases according to the features of uplifting-depression change and the palaeogeographic property in Xuefeng a... |
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| Keywords: | intracontinental orogenic belt Xuefeng uplift sedimentary evolution |
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