必须声明标量变量 "@Script_ID"。 内蒙古雅布赖盆地红柳沟中侏罗统沉积相及沉积环境研究-《地球科学与环境学报》
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[1]钟福平,钟建华,由伟丰,等.内蒙古雅布赖盆地红柳沟中侏罗统沉积相及沉积环境研究[J].地球科学与环境学报,2010,32(02):149-154.
 ZHONG Fu-ping,ZHONG Jian-hua,YOU Wei-feng,et al.Study on Sedimentary Facies and Environment of Middle Jurassic in Hongliugou of Yabulai Basin, Inner Mongolia[J].Journal of Earth Sciences and Environment,2010,32(02):149-154.
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内蒙古雅布赖盆地红柳沟中侏罗统沉积相及沉积环境研究(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第32卷
期数:
2010年第02期
页码:
149-154
栏目:
基础地质与矿产地质
出版日期:
2010-06-20

文章信息/Info

Title:
Study on Sedimentary Facies and Environment of Middle Jurassic in Hongliugou of Yabulai Basin, Inner Mongolia
文章编号:
1672-6561(2010)02-0149-06
作者:
钟福平12钟建华13由伟丰4王勇1张磊3边强5艾合买提江·阿不都热和曼3高玉飞3王金华3
(1.中国科学院 广州地球化学研究所,广东 广州 510640; 2.中国科学院 研究生院,北京 100049; 3.中国石油大学 地球资源与信息学院,山东 东营 257061; 4.中国石油化工股份有限公司 石油勘探开发研究院,北京 100083; 5.中国人民解放军空军95338部队 1大队,湖南 衡阳 421200)
Author(s):
ZHONG Fu-ping12 ZHONG Jian-hua13 YOU Wei-feng4 WANG Yong1 ZHANG Lei3 BIAN Qiang5 Ahmatjan ABDURAHMAN3 GAO Yu-fei3 WANG Jin-hua3
(1.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China; 2.Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3.School of Geo-resources andInformation, China University of Petroleum, Dongying 257061, Shandong, China; 4.Research Institute of Oil Exploration and Development, China Petroleum and Chemical Corporation, Beijing 100083, China; 5.Team 1,Troop 95338, the Air Force of the Chinese People's Liberation Army, Hengyang 421200, Hunan, China)
关键词:
中侏罗统沉积相沉积环境青土井组雅布赖盆地红柳沟
Keywords:
Middle Jurassic sedimentary facies sedimentary environment Qingtujing Formation Yabulai Basin Hongliugou
分类号:
P586;P588.2
DOI:
-
文献标志码:
A
摘要:
野外考察发现,雅布赖盆地红柳沟发育一套较完整的中侏罗统扇三角洲沉积地层。其中沉积亚相有扇三角洲平原、扇三角洲前缘及前扇三角洲亚相;沉积微相包括辫状河道、天然堤、决口、沼泽、水下分流河道、水下分流河道间、河口坝、席状砂等沉积微相。从沉积构造特征分析可以看出,河道沉积发育于水动力条件较强的沉积环境,扇三角洲前缘河口坝沉积发育于强与弱水动力条件交替出现的沉积环境,而前扇三角洲则在比较稳定的水动力条件下沉积。对野外6个泥岩样品的微量元素化验结果用蜘蛛图解分析处理,得到样品所含微量元素V、Sr、Rb、B相对富集,而Zr、Cr、Ni相对亏损。通过对该地区样品w(Fe2+)/w(Fe3+)及气候指数计算表明,当时为弱氧化、半干旱的沉积环境。
Abstract:
Based on the field investigation in Hongliugou of Yabulai Basin, the results indicate that the main sedimentary facies is Jurassic fan delta, which can be divided into three subfacies including fan delta plain, fan delta front and pre-fan delta and six microfacies including braided channel, natural levee, crevasse, marsh, underwater distributary channel, underwater distributary interchannel, mouth bar, sheet sand, and so on. According to the field characteristics of sedimentary structures, the channel deposits developed in the condition of strong hydrodynamic, mouth bar deposits of fan delta front developed in the condition of alternating dynamic of strong and weak, and the pre-fan delta developed in the condition of relatively stable hydrodynamic. According to the analysis of trace elements in six samples of mudstone with spider diagrams, the results show that the contents of V, Sr, Rb, B are relatively high, but Zr, Cr, Ni are relatively low. Calculations of climate index and the ratio of mass factions of Fe2+ and Fe3+ show that the sedimentary environment was weak oxidation and semi-arid in Middle Jurassic.

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备注/Memo

备注/Memo:
收稿日期:2009-07-23
基金项目: 国家重点基础研究发展计划项目(2006CB202406); 中国石油化工股份有限公司项目(07370502000130)
作者简介: 钟福平(1978-),男,江西分宜人,理学博士研究生,从事油气成藏研究。E-mail:zhongfp-2022@163.com
更新日期/Last Update: 2010-06-20