| 鄂尔多斯盆地柳林地区下奥陶统冶里组竹叶状石灰岩的沉积环境和成因机制 |
| |
| 引用本文： | 王千遥,冯乔,贾凌云,刘阵,赵伟,周书昌. 鄂尔多斯盆地柳林地区下奥陶统冶里组竹叶状石灰岩的沉积环境和成因机制[J]. 沉积与特提斯地质, 2010, 30(4): 55-59 |
| |
| 作者姓名： | 王千遥 冯乔 贾凌云 刘阵 赵伟 周书昌 |
| |
| 作者单位： | 山东省沉积成矿作用与沉积矿产重点实验室山东科技大学地质科学与工程学院 |
| |
| 摘 要： | 鄂尔多斯盆地柳林地区早奥陶世冶里期沉积以浅灰色中薄层泥质白云岩为主,发育大量竹叶状碳酸盐岩。不同类型的竹叶状碎屑反映了不同的沉积环境。笔者对研究区剖面内的竹叶状碎屑进行分析和研究后认为,竹叶状石灰岩的形成可以分为早期沉积物的形成和早期沉积物的破碎、搬运和再沉积两个阶段。
|
| 关 键 词： | 竹叶状石灰岩 风暴 破碎 奥陶系 鄂尔多斯盆地 |
Sedimentary environments and genesis of edgewise limestones:An example from the Lower Ordovician Yeli Formation in the Ordos Basin |
| |
| WANG Qian-yao,FENG Qiao,JIA Ling-yun,LIU Zhen,ZHAO Wei,ZHOU Shu-chang. Sedimentary environments and genesis of edgewise limestones:An example from the Lower Ordovician Yeli Formation in the Ordos Basin[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(4): 55-59 |
| |
| Authors: | WANG Qian-yao FENG Qiao JIA Ling-yun LIU Zhen ZHAO Wei ZHOU Shu-chang |
| |
| Affiliation: | Shandong Key Laboratory of Depositional Mineralization and Sedimentary Minerals,College of Geological Science and Engineering,Shandong University of Science and Technology,Qingdao 266510,Shandong,China |
| |
| Abstract: | The sedimentary strata in the Lower Ordovician Yeli Formation,Liulin,Ordos Basin dominantly consist of light grey medium-to thin-bedded muddy dolostones,with well-developed edgewise carbonate rocks.These edgewise limestones have experienced two stages of formation,including the deposition of sediments in the early stage,and then fracturing,transport and redeposition of the sediments. |
| |
| Keywords: | edgewise limestone storm fracturing Ordovician Ordos Basin |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《沉积与特提斯地质》浏览原始摘要信息 |
|
点击此处可从《沉积与特提斯地质》下载免费的PDF全文 |
