|
|||||
|
|
| 中扬子中侏罗统陆相高分辨率层序 地层格架及构造控制 | |
| 引用本文： | 段凯波.中扬子中侏罗统陆相高分辨率层序 地层格架及构造控制[J].地质与勘探,2012,48(2):406-414. |
| 作者姓名： | 段凯波 |
| 作者单位： | 1. 中国地质大学（北京）地球科学与资源学院,北京100083／中国地质大学（北京）地质过程与矿产资源国家重点实验室,北京100083／中化地质矿山总局化工地质调查总院,北京100101 2. 中化地质矿山总局化工地质调查总院,北京,100101 3. 中国地质大学（北京）地球科学与资源学院,北京100083／中国地质大学（北京）地质过程与矿产资源国家重点实验室,北京100083 |
| 基金项目： | 本文为中国石油化工股份有限公司科技工程重点项目(编号QZ-2005 -06) 和国家自然科学基金(编号49803012 和 40472065)资助的成果 |
| 摘 要： | 摘 要] 中扬子中侏罗统主要散布于中扬子前陆盆地各次级盆地中,应用现代沉积学、高分辨率层序地层学理论,结合露头岩性、古生物、沉积相分析等手段,发现中侏罗统主要为辫状河、辫状河三角洲或扇三角洲以及滨浅湖沉积体系,在不同区域,分别以花家湖组、沙溪庙组和千佛崖组地层命名。不同区域层序特征既有差异,又存在相似性。根据高分辨率层序地层学理论,将花家湖组、沙溪庙组和千佛崖组分别划分为4 个、4个和2个三级层序,局部地区还可细划四级层序,整个中侏罗统大致相当于1个二级层序。此层序地层格架的形成主要是受构造因素控制,即印支期以来中扬子地区发生强烈的构造变形和运动而形成复杂的盆山耦合体系,层序横向展布和纵向叠加于前陆盆地中。 |
| 关 键 词： | 找矿模型 三维找矿 深部隐伏矿体 云南个旧 |
| 收稿时间： | 2010/10/11 0:00:00 |
| 修稿时间： | 7/6/2011 12:00:00 AM |
Continental High-resolution Sequence Stratigraphic Framework of the Middle Jurassic System in the Middle Yangtze Region and Tectonic Controls |
|
| DUAN Kai-bo.Continental High-resolution Sequence Stratigraphic Framework of the Middle Jurassic System in the Middle Yangtze Region and Tectonic Controls[J].Geology and Prospecting,2012,48(2):406-414. | |
| Authors: | DUAN Kai-bo |
| Institution: | School of Earth-Sciences and Resources,China University of Geosciences (Beijing),Beijing |
| Abstract: | Abstract: The middle Jurassic System of the Middle Yangtze region is mainly distributed in some sub-basins of the Middle Yangtze foreland basin. This work is based on principles of modern sedimentology and high - resolution sequence stratigraphy in combination with analysis of outcrop lothology,paleontology and sedimentary facies. The result shows that this System is characterized by braided river,braided-river delta,fan delta,and shallow lake sediments,and has named as the Huajiahu Formation,Shaximiao Formation and Qianfuya Formation for varied areas. Sequence stratigraphic characteristics of different regions exhibit both differences and similarities. Based on the theory of high-resolution sequence stratigraphy,the Huajiahu Formation,Shaximiao Formation and Qianfuya Formation can be respectively divided into 4,4 and 2 third-order sequences. Furthermore,fourth-order sequences can be subdivided in local areas. The whole Middle Jurassic System is roughly equivalent to a second-order sequence. The formation of this sequence stratigraphic framework is primarily controlled by the tectonic factors,i. e. the intensive tectonic deformation and movement since the Indosinian period,which resulted in a complicated basin-mountain coupling system that made the sequences distributed laterally and superimposed longitudinally in the foreland basin. |
| Keywords: | Middle Yangtze region middle Jurassic high-resolution sequence framework tectonic controls |
| 本文献已被 CNKI 万方数据 等数据库收录！ | |
| 点击此处可从《地质与勘探》浏览原始摘要信息 | |
| 点击此处可从《地质与勘探》下载免费的PDF全文 | |