|本期目录/Table of Contents|

[1]王伟.东濮凹陷文南—刘庄地区沙二下亚段浅湖风暴沉积[J].地球科学与环境学报,2011,33(04):384-389.
　WANG Wei.Storm Deposits of Shallow Lake in Lower Submember of Member 2 of Shahejie Formation of Wennan-Liuzhuang Area,Dongpu Sag[J].Journal of Earth Sciences and Environment,2011,33(04):384-389.
点击复制

东濮凹陷文南—刘庄地区沙二下亚段浅湖风暴沉积(PDF)
分享到：

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第33卷
期数:
2011年第04期
页码:
384-389
栏目:
基础地质与矿产地质
出版日期:
2011-12-15

文章信息/Info

Title:
Storm Deposits of Shallow Lake in Lower Submember of Member 2 of Shahejie Formation of Wennan-Liuzhuang Area,Dongpu Sag
文章编号:
1672-6561(2011)04-0384-06
作者:
王伟
中国石油化工股份有限公司胜利油田公司地质科学研究院,山东东营257015
Author(s):
WANG Wei
Geological Scientific Research Institute, Shengli Oilfield, China Petroleum and Chemical Corporation,Dongying 257015, Shandong, China
关键词:
风暴沉积; 鲍马序列; 沙二下亚段; 古近系; 浅水湖盆; 东濮凹陷
Keywords:
storm deposit;  Bouma Sequence;  lower submember of member 2 of Shahejie Formation;  Paleogene;  shallow water lake;  Dongpu Sag
分类号:
TE121.3;P618.13
DOI:
-
文献标志码:
A
摘要:
风暴沉积是一种特殊的事件沉积,反映了区域特定时期的古地理环境和古气候变化。通过区域古地理研究和精细地层对比,探讨了东濮凹陷文南—刘庄地区沙二下亚段沉积时期浅湖风暴沉积证据及特征,在此基础上总结了风暴沉积模式。结果表明:沙二下亚段沉积时期湖盆沉积层序主要受气候条件控制,气候频繁变化导致风暴沉积广泛分布、多期发育;风暴沉积主要发育在湖侵体系域和高水位体系域,沉积早期发育在深水区,而到沉积晚期分布范围扩大;风暴沉积一般发生在每期砂组的边界附近,作为短期、等时的一种事件沉积,可以用来作为层序划分的辅助标志;研究区风暴沉积模式主要有I类和II类两种;I类风暴沉积为类深水风暴沉积,发育A—D段沉积的类鲍马序列层序,但粒度要较深水风暴沉积细得多,多见于漫湖沉积环境相对深水区;II类风暴沉积不发育I类风暴的B和D段沉积;风暴流在风暴停止时越靠近湖盆中央,其沉积特征就越类似深水风暴沉积,反之则越类似II类风暴沉积。
Abstract:
Storm deposit is a kind of special event deposit, and reveals palaeogeography and palaeoclimatology changes of certain period in certain region. Through the palaeogeography research and fine strata division, the evidence and characteristic of storm deposit of shallow lake in lower submember of member 2 of Shahejie Formation of Wennan-Liuzhuang Area, Dongpu Depression were discussed, and the sedimentary model of storm deposit was summarized. The results showed that deposition sequence of lake basin was mainly controlled by climate, so the frequent climate change resulted in the wide distribution and multi-period development of storm deposit; storm deposit mainly developed in lake transgressive system tract(TST)and highstand system tract(HST), and developed in deep water during the early deposit, and the distribution range enlarged during the later deposit; storm deposit, which could be the assistant mark for strata sequence division, generally occurred around the boundary of each sand group, and was taken as a event deposit with short term and isochronous; the sedimentary models of storm deposit mainly included class I and class II; class I storm deposit was similar to that developed in deep water, and developed A-D interval deposits which was similar to Bouma Sequence, but the granularity was thinner than that of storm deposit developed in deep water, and mostly developed in relatively deep water of flood-over-lake depositional environment; class II storm deposit did not develop the B and D interval deposits; when the storm stopped, if the storm flow was closer to the center of lake basin, the sedimentary characteristic was more similar to class I storm deposit, otherwise, it was more similar to class II.

参考文献/References:

[1] 李宗信,张国栋.文南油田文33块沙二下亚段沉积微相与储层研究[R].河南濮阳:中国石油化工股份有限公司中原油田公司勘探开发科学研究院,1993.
[2] 纪友亮,冯建辉,王声朗,等.东濮凹陷下第三系沙三段盐岩和膏盐岩的成因[J].沉积学报,2005,23(2):225-231.
[3] 周新科,许化政.东濮凹陷地质特征研究[J].石油学报,2007,28(5):20-26.
[4] 王 伟,张世奇,纪友亮.青坨子凸起馆陶组地震相研究[J].断块油气田,2007,14(1):16-18.
[5] 纪友亮,张世奇.层序地层学原理及层序成因机制模式[M].北京:地质出版社,1998.
[6] 倪新锋,陈洪德,赵俊兴,等.陆相层序界面的物质表现及成因类型——以鄂尔多斯盆地中生界为例[J].地球科学与环境学报,2007,29(3):256-262.
[7] 王 伟.东营凹陷青坨子凸起馆陶组沉积相演化特征及相模式[J].石油天然气学报,2009,31(3):167-170.
[8] Ager D V.Storm Deposits in the Jurassic of the Moroccan High Atlas [J].Palaeogeography,Palaeoclimatology,Palaeoecology,1974,15(2):83-93.
[9] Kreisa R D.Storm-generated Sedimentary Structures in Subtidal Marine Facies with Examples from the Middle and Upper Ordovician of Southwestern Virginia[J].Journal of Sedimentary Research,1981,51(3):823-848.
[10] Wnuk C,Pfefferkorn H W.A Pennsylvanian-age Terrestrial Storm Deposit:Using Plant Fossils to Characterize the History and Process of Sediment Accumulation[J].Journal of Sedimentary Research,1987,57(2):212-221.
[11] 钱 峥,李 淳,马在平.安徽巢北地区下石炭统高骊山组风暴沉积[J].石油大学学报:自然科学版,1996,20(5):8-11.
[12] 杜远生,韩 欣.滇中中元古代昆阳群因民组碎屑风暴岩及其意义[J].沉积学报,2000,18(2):259-262.
[13] 杨瑞东 赵元龙 毛家仁,等.贵州台江中寒武世凯里生物群古生态研究[J].沉积学报,2002,20(1):129-134.
[14] 姜在兴,赵澂林,刘孟慧,等.东濮凹陷西部湖相风暴沉积的初步研究[J].沉积学报,1990,8(1):107-114.
[15] 袁 静.惠民凹陷古近系风暴沉积研究[J].中国石油大学学报:自然科学版,2006,30(4):1-6.
[16] 赵澂林,刘孟慧,纪友亮.东濮凹陷下第三系碎屑岩沉积体系与成岩作用[M].北京:石油工业出版社,1992.
[17] 田翠翠,余克服.古风暴研究进展[J].海洋地质与第四纪地质,2011,31(4):171-177.
[18] 杨宝忠,杨坤光,夏文臣.鄂东黄石地区下三叠统大冶组风暴沉积[J].古地理学报,2007,9(4):379-386.
[19] 马瑞申,张 良,杜远生,等.豫北地区寒武系风暴岩沉积特征及其地质意义[J].地质科技情报,2011,30(4):15-20.
[20] 王 伟,王锦程,李 博.东海平湖油气田八角亭构造区H4段沉积展布特征和相模式研究[J].地层学杂志,2011,35(4):448-453.
[21] 徐春强,蒋有录,程 奇,等.东濮凹陷濮卫洼陷油气成藏期分析[J].地球科学与环境学报,2010,31(3):257-262.
[22] 丁晓琪,张哨楠.层序地层学在河流相地层研究中的应用[J].西安石油大学学报:自然科学版,2010,25(4):1-5.
[23] 董 洁,陈世悦,李 聪.辽河西部凹陷欢喜岭地区沙河街组三段层序地层与沉积相研究[J].地球科学与环境学报,2010,32(3):245-251.
[24] 蔡 佳,王 华,罗家群.基于层序地层格架的南阳凹陷油气成藏模式[J].西南石油大学学报:自然科学版,2011,33(3):67-73.
[25] 田景春,张 翔,许 珉,等.南华北盆地青白口系—侏罗系层序界面时空分布特征研究[J].地球科学与环境学报,2010,32(4):331-337.
[26] Marsaglia K M,Klein G D.The Paleogeography of Paleozoic and Mesozoic Storm Depositional Systems[J].Journal of Geology,1983,91(2):117-142.
[27] 王 伟,张世奇,纪友亮.环胶州湾海岸线演化与控制因素[J].海洋地质动态,2006,22(9):7-10.
[28] 刘 奇 宋传中,崔 王,等.淮河源区中更新世黄土堆积的元素地球化学特征及其古气候意义[J].地球科学与环境学报,2007,29(4):356-361.
[29] 王 伟.张屯嘴—丁家嘴沿岸现代沉积和水动力研究[J].海洋地质动态,2010,26(2):25-31.[0] 《地球科学与环境学报》连续第三次荣获 “中国科技论文在线优秀期刊”二等奖 据教育部科技发展中心消息,《地球科学与环境学报》荣获2010年度“中国科技论文在线优秀期刊”二等奖。这是本刊继获得2008年度和2009年度“中国科技论文在线优秀期刊”二等奖之后第三次获此殊荣。 为了促进科技期刊健康发展,提高科技期刊的质量,推动科技期刊的数字化建设,提高期刊刊载论文的引用率,扩大期刊的影响力,促进论文免费共享,建设良好的科研环境,使科技期刊更好地为科研和科研工作者服务,根据教技发中心函

相似文献/References:

备注/Memo

备注/Memo:
收稿日期:2011-01-29
基金项目: 中国石油化工股份有限公司胜利油田公司科研项目(06370502000045); 国家重点基础研究发展计划项目(2006CB202302)
作者简介: 王 伟(1981-),男,山东聊城人,工程师,工学硕士,从事油气藏勘探开发研究。E-mail:kinvey@163.com

更新日期/Last Update: 2011-12-20