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| 鲁西南地区官庄群沉积特征与沉积环境分析 | |
| 引用本文： | 郑德顺,李明龙,李守军.鲁西南地区官庄群沉积特征与沉积环境分析[J].沉积与特提斯地质,2012,32(4):1-7. |
| 作者姓名： | 郑德顺 李明龙 李守军 |
| 作者单位： | 1. 河南理工大学资源与环境工程学院,河南 焦作454000;中国地质大学“构造与油气资源”教育部重点实验室,湖北 武汉430074 2. 河南理工大学资源与环境工程学院,河南 焦作,454000 3. 山东科技大学地球信息科学与工程学院,山东 青岛,266510 |
| 基金项目： | 国家自然科学基金项目(40902033);中国地质大学“构造与油气资源”教育部重点实验室项目开放研究基金(TPR-2010-24);河南理工大学博士基金项目(B2009-93)联合资助 |
| 摘 要： | 鲁西南地区上白垩统—始新统主要发育官庄群,前人对该群的研究大多集中于地层归属年代的划分上,而对于沉积环境的分析涉及较少。本文主要运用岩石学、沉积地球化学方法对鲁西南地区平邑盆地广阜庄-挑沟剖面地层沉积特征及沉积环境演化进行了研究。结果表明:官庄群的固城组为陆相河湖碎屑岩沉积,卞桥组为浅湖碳酸盐岩和蒸发岩沉积,常路组以滨浅湖碳酸盐岩沉积为主,朱家沟组为一套山麓洪积扇沉积;卞桥组和常路组碳酸盐岩总体属于高盐度、强蒸发的陆相咸化湖泊环境沉积产物;官庄群沉积旋回的发育主要受蒙山断裂的多期次活动及古气候条件控制。 |
| 关 键 词： | 沉积环境 沉积地球化学 官庄群 鲁西南地区 |
| 收稿时间： | 2011/10/26 0:00:00 |
| 修稿时间： | 2011/12/5 0:00:00 |
Sedimentary characteristics and environments of the Guanzhuang Group in southwestern Shandong |
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| ZHENG De-shun,LI Ming-long,LI Shou-jun.Sedimentary characteristics and environments of the Guanzhuang Group in southwestern Shandong[J].Sedimentary Geology and Tethyan Geology,2012,32(4):1-7. | |
| Authors: | ZHENG De-shun LI Ming-long LI Shou-jun |
| Institution: | 1.School of Resources and Environment Engineering,Henan Polytechnic University,Jiaozuo 454000,Henan,China;2.Key Laboratory of Tectonics and Petroleum Resources under the Ministry of Education,China University of Geosciences,Wuhan 430074,Hubei,China;3.College of Geo-info Sciences and Engineering,Shandong University of Science and Technology,Qingdao 266510,Shandong,China) |
| Abstract: | The Upper Cretaceous-Eocene Guanzhuang Group is well developed in southwestern Shandong. The previous studies were once concentrated mainly in stratigraphic division and correlation, and scarcely in sedimentary environmental analysis. The present paper focuses on the sedimentary characteristics and environments of the Guangfuzhuang-Tiaogou section in the Pingyi Basin on the basis of petrological and geochemical examination. In the Guanzhuang Group, there occur the continental fluviolacustrine clastic rocks in the Gucheng Formation; shallow lacustrine carbonate rocks and evaporates in the Bianqiao Formation; littoral-shallow lacustrine carbonate rocks in the Changlu Formation, and pediment fluvial fan deposits in the Zhujiagou Formation. The carbonate rocks in the Bianqiao and Changlu Formations were laid down in the highly saline and highly evaporative continental salinized lake environments. The depositional cycles in the Guanzhuang Group are generally controlled by the multiphase faulting of the Mengshan fault and palaeoclimatic changes. |
| Keywords: | sedimentary environment sedimentary geochemistry Guanzhuang Group southwestern Shandong |
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