| 单县矿区高分辨率层序地层及成煤作用研究 |
| |
| 引用本文： | 吕大炜,梁吉坡,李增学,王薇,吴立荣,张义江,郭建斌,宋洪柱.单县矿区高分辨率层序地层及成煤作用研究[J].地球学报,2008,29(5):633-638. |
| |
| 作者姓名： | 吕大炜 梁吉坡 李增学 王薇 吴立荣 张义江 郭建斌 宋洪柱 |
| |
| 作者单位： | 山东科技大学，山东青岛266510;山东省地质科学实验研究院，山东济南250013;山东科技大学，山东青岛266510;山东省地质科学实验研究院，山东济南250013;山东科技大学，山东青岛266510;山东省地质科学实验研究院，山东济南250013;山东科技大学，山东青岛266510;山东科技大学，山东青岛266510 |
| |
| 基金项目： | 国家重点基础研究发展计划(973计划)项目(编号:2003CB214608); 2008年山东科技大学研究生科技创新基金 |
| |
| 摘 要： | 运用高分辨率层序地层原理,通过岩心、测井资料的综合分析,对研究区上古生界进行了不同周期地层基准面旋回研究,识别出短期、中期、长期及超长期4种规模的地层旋回。通过对比分析,建立了该区高分辨率层序地层格架。研究表明,研究区成煤作用出现于基准面旋回的特殊位置(A/S接近于1),当叠置在长期基准面旋回下降半旋回和中期基准面旋回下降半旋回晚期是成煤的最有利时期。根据盆地充填演化和不同级次基准面旋回叠加可以将研究区成煤作用分为早期成煤作用和晚期成煤作用,依次分析了不同时期成煤作用的地层基准面变化和盆地沉积充填演化的过程。
|
| 关 键 词： | 高分辨率层序地层 基准面旋回 成煤作用 单县矿区 |
A Study of High-resolution Sequence Stratigraphic Characteristics and Coal Accumulation in Upper Paleozoic Strata of the Shanxian Coalfield |
| |
| Institution: | Shandong University of Science and Technology, Qingdao, Shandong 266510;Geological Institute of Shandong Province, Jinan, Shandong 250013;Shandong University of Science and Technology, Qingdao, Shandong 266510;Geological Institute of Shandong Province, Jinan, Shandong 250013;Shandong University of Science and Technology, Qingdao, Shandong 266510;Geological Institute of Shandong Province, Jinan, Shandong 250013;Shandong University of Science and Technology, Qingdao, Shandong 266510;Shandong University of Science and Technology, Qingdao, Shandong 266510 |
| |
| Abstract: | Based on the principle of high-resolution sequence stratigraphy and an integrated analysis of the bore core and well logging, the authors divided different base level cycles of Upper Paleozoic strata in the study area. Four types of base level cycles were recognized: short, intermediate, long and extremely long. Through a comparative analysis, a high-resolution sequence framework was established. Researches show that the most favorable coal accumulation of the study area occurred at the special positions of the base level cycles (A/S close to 1), i.e., at the half level of the descending long base level and the late stage of the descending half level of the middle base level. According to the basin filling and the superimposition of different classes of base levels, the coal accumulation of the study area can be divided into early accumulation and late accumulation. The base level change of both accumulations and the course of basin filling evolution are analyzed in this paper. |
| |
| Keywords: | high-resolution sequence stratigraphy base level cycle coal accumulation Shanxian coalfield |
| 本文献已被 万方数据 等数据库收录！ |
| 点击此处可从《地球学报》浏览原始摘要信息 |
| 点击此处可从《地球学报》下载免费的PDF全文 |
|
