必须声明标量变量 "@Script_ID"。 鄂尔多斯盆地中部上古生界沉积相演化-《地球科学与环境学报》
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[1]张晓莉.鄂尔多斯盆地中部上古生界沉积相演化[J].地球科学与环境学报,2005,27(03):26-29,37.
 ZHANG Xiao-li.Sedimentary facies evolution of Upper Palaeozoic formation in Ordos Basin[J].Journal of Earth Sciences and Environment,2005,27(03):26-29,37.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第27卷
期数:
2005年第03期
页码:
26-29,37
栏目:
出版日期:
2005-09-15

文章信息/Info

Title:
Sedimentary facies evolution of Upper Palaeozoic formation in Ordos Basin
作者:
张晓莉
长安大学地球科学与国土资源学院,陕西西安710054
Author(s):
ZHANG Xiao-li
School of Earth Sciences and Resources Management,Chang’ an University,Xi’ an 710054,China
关键词:
鄂尔多斯盆地沉积相沉积演化生储盖组合
Keywords:
Ordos Basin sedimentary facies sedimentary evolutionsource-reservoir-cap rock combinations
分类号:
P618.130.2
DOI:
-
文献标志码:
A
摘要:
利用钻井资料和地质资料对鄂尔多斯盆地上古生界沉积相演化进行详细的研究,分析了本溪期 (海侵)、太原期(海侵扩大)、山西期(海退)、石盒子期(海陆交互)和石千峰期(陆缘湖泊)等5个时期的古 地理环境、岩石类型、沉积相类型和平面展布特征,得出这5个时期在盆地内构成了一个海侵海退旋回,形 成了从滨浅海相到海陆过渡的三角洲相、河流湖泊相陆源沉积。控制生成了三角洲相分流河道砂砾岩、水 下分流河道砂砾岩以及潮坪相砂坝等有利储集岩带,潮坪相发育的煤系地层为烃源岩,上石盒子组洪泛平 原形成泥质岩盖层。生油岩和储集岩叠置或互侧式组合关系,形成本区受砂体分布控制的岩性气藏。
Abstract:
This study of sedimentary facies evolution of the Upper Palaeozoic formation is based on drilling and geological in- formation.It analyses palaeogeographic environment, rock type,sedimentary facies type and distribution in the Benxi Stage (incursion), Taiyuan Stage(incursion spread), Shanxi Stage(regression),Shihezi Stage(paralic) and Shiqianfeng Stage (continental lacustrine).As a result,these five stages formed a transgression and regrssive cycle including from coastal facies to delta facies,fluvial facies and lacustrine facies of continental sedimentary in marine-continental transition,and controlled the formation of the favorable reservoir facies which comprised delta facies distributary chanel psepholite,submerged distrib- utary chanel psepholite and tidal flat facies bar.The hydrocarbon source rocks is coal-bearing strata in the tidal flat facies. The caprock is related to shaly rocks in the flood plain.The complicated overlapping and juxtaposition between the source and reservoir rocks caused the formation of lithologic gasses, which was largely controlled by sandbody distribution.

参考文献/References:

[1] 杨俊杰. 鄂尔多斯盆 地构造演 化与油气 分布规律[M] . 北京 : 石油工业出版社 , 2002.
[2] 汪正江 , 陈洪德 , 张锦泉 , 等. 鄂尔多斯盆地二叠纪 煤成气成藏 特征[J] . 矿物岩石 , 2002 , 22(3):47 ~ 52.
[3] 钱锋 , 艾永峰. 鄂尔多斯 南部地区 早古生代 主动大陆 边缘演 化特征[J]. 西安工程学院学报 , 2002 , 24(1):18 ~ 21.
[4] 王平 , 周义 , 季海锟. 靖安油田北东区局部构造与 石油富集关 系研究[J] . 长安 大学学 报(地 球科学 版), 2003 , 25(4):10 ~ 13.
[5] 杨仁超 , 韩作振 , 李文厚 , 等. 鄂尔多斯地区二叠系 三角洲沉积 特征及其模式[J] . 西北大学学报(自然科学版), 2004 , 34(3): 340 ~ 344.
[6] 肖建喜. 鄂尔多斯盆地西缘北段上古生界储集层研究[J]. 西 北大学学报(自然科学版), 2003 , 33(2):201 ~ 204.

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备注/Memo

备注/Memo:
[收稿日期]2005-01-18
[作者简介]张晓莉(1970-),女,陕西华县人,讲师,从事石油地质教学与研究。
更新日期/Last Update: 1900-01-01