| 山东尚南断块古近系东营组沉积相及其古地理? |
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| 引用本文： | 毕义泉.山东尚南断块古近系东营组沉积相及其古地理?[J].古地理学报,2002,4(3):19-25. |
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| 作者姓名： | 毕义泉 |
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| 作者单位： | 中国石化化工股份有限公司胜利油田分公司，山东东营 257001 |
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| 基金项目： | 中国石油化工集团公司“九五”攻关项目老区油田提高采收率技术研究 (980 316 )资助 |
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| 摘 要： | 尚南断块位于山东省胜利油田东营凹陷尚店油田西南部。该区的古近系东营组顶底均为不整合面或沉积间断面，发育了较好的湖侵三角洲相沉积。基于100余口钻井、地震资料，70多张单井剖面柱状图编制及14条剖面的对比，进行了东营组精细沉积相研究，编制出30余幅沉积微相投点图和岩相古地理图。研究表明，东营 沉积时期气候潮湿、雨水丰沛、河流纵横、湖泊扩大、湖水变深等为处于斜坡地区的尚南地区发育湖侵期三角洲提供了良好的条件。控制该区沉积和地层发育的区域性物源来自埕宁隆起和鲁西隆起，但来自滨县凸起和林樊家突起的局部物源也有很大影响。东营期岩相古地理经历了早、中、晚期的演化，早期发育了以三角洲平原为主的沉积环境，中期形成了大范围的破坏性三角洲环境，晚期以前三角洲环境为特色。
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| 关 键 词： | 山东 古近系 尚南断块 东营组 沉积相 古地理 三角洲沉积 |
| 文章编号： | 1671-1505(2002)03-0019-07 |
| 修稿时间： | 2002年3月1日 |
SEDIMENTARY FACIES AND PALAEOGEOGRAPHY OF DONGYING FORMATION OF PALEOGENE OF SOUTH SHANGDIAN FAULT BLOCK IN SHANDONG PROVINCE |
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| Bi Yiquan Shengli Oilfield Division of China Petroleum and Chemical Corporation,Dongying ,Shandong.SEDIMENTARY FACIES AND PALAEOGEOGRAPHY OF DONGYING FORMATION OF PALEOGENE OF SOUTH SHANGDIAN FAULT BLOCK IN SHANDONG PROVINCE[J].Journal of Palaeogeography,2002,4(3):19-25. |
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| Authors: | Bi Yiquan Shengli Oilfield Division of China Petroleum and Chemical Corporation Dongying Shandong |
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| Institution: | Shengli Field Division of China Petroleum and Chemical Corporation, Dongying 257001，Shandong |
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| Abstract: | The south Shangdian fault block is located at the Shangdian Oilfield of Dongying Depression in Shengli Oilfield in Shandong Province. The Dongying Formation of the Paleogene is well defined by unconformity or discontinuous surface both at its top and bottom. Within this Formation, some delta deposits were developed due to lacustrine transgression. Based on the drilling log and seismic studies of over 100 wells, columnar maps of over 70 sections of single well and correlations of 14 sections in the Shangnan faulted block, the sedimentary facies of the Dongying Formation are well studied. More than 30 casting-dot maps of sedimentary microfacies and lithofacies palaeogeographic maps are designed. The results show that in the Dongying Age, the environment of flourish rainfall, moist climate, abundant rivers and lakes, and so on was favorable to developing lacustrine transgressive delta.Although the regional source areas, the Chengning uplift and Luxi uplift, might play an important role in controlling the sedimentary envirenment and sequence development,the local source areas,such as the Binxian and Linfanjia arch also play an important role in the delta development. There were three evolutional stages of lithofacies palaeogeography during the Dongying Age , including the Early, Middle and Late Age . During the Early Age, the sedimentary environment of delta plain predominated. In the Middle Age, the destructed delta was developed. In the Late Age, the foredelta was characterized. |
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| Keywords: | south Shangdian fault block Dongying Formation sedimentary facies palaeogeography delta facies deposition |
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