|Table of Contents|

Relationship Between Pre-Jurassic Palaeogeomorphology and Oil Distribution of Zhenjing Oilfield in South Ordos Basin(PDF)

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

Issue:
2008年第04期
Page:
385-
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Relationship Between Pre-Jurassic Palaeogeomorphology and Oil Distribution of Zhenjing Oilfield in South Ordos Basin
Author(s):
DING Xiao-qiZHANG Shao-nanLIU Yan
State Key Laboratory o f Oil and Gas Reservoir Geology and Exploitation, Chengdu University o f Technology, Chengdu 610059, Sichuan, China)
Keywords:
Zhenjing oilfield method of mold palaeogeomorphology compacting efficiency
PACS:
TE121.3
DOI:
-
Abstract:
Pre-Jurassic palaeogeomorphology of Zhenjing oilfield has been mapped by mold method according to well cores, cast liquid photos and petrophysical data, as well as interpretation of well logs. Based on analysis of palaeogeomorphology, it is found that the distribution of sedimentary facies of Yan 9 formation was controlled by pre-Jurassic palaeogeomorphology, braid channels flew out the valley from highland with gentle slopes, and some distributaries of braid channels in the north part came to braid channel in the south.The structures of Yan 9 were formed by differential compaction. Highland and ridge could formed comparative high angle anticline easily. The petrophysics of Chang 6 formation under the denudation plane were controlled by leaching degree, that is to say, reservoir has better petrophysics if it experienced strong leaching through which the products of alteration were discharged easily. The degree of leaching and discharge of alteration products were controlled by palaeomorphology, thus, valley had most leaching zones.The Yan 9 reservoir over the denudation plane were controlled by structures and sandstones, and oils distributed in highland and ridge. However, the Chang 6 reservoir under the denudation plane were controlled by degree of leaching, and oils distributed in valley.

References:

[1] Troutman T J .Reservoir C haracterizati on , Paleoen vi ronment , and Pl aeomorphology of the Mi ssissippian Redw all Lim es tone Paleokarst , Hu alapai Indian Reservoi r , G rand Canyon Area , Arizona[J] .AAPG Bulletin , 2000 , 84(11): 1875-1883 .
[2] H ouse M A ,Wernicke B P, Farley K A .Paleogeomorphology of the Cent ral and Sou thern Sierra Nevada:Fu rther In si ght s f rom Apati te(U-Th)/ He Ages[J] .Geological Societ y of America , 1999 , 31(7):481-482 .
[3] Sangst er D F .Paleogeomorphology in the Explo rat ion f or Undi scovered S andst one-Lead Deposits , Salmon River Basin , Nova Scotia[J] .CIM Bull et in , 1990 , 83(4):62-68 .
[4] 宋 凯 ,吕剑文 ,凌升阶 ,等 .鄂尔多斯盆地定边 —吴旗地区前 侏罗纪古地貌与油藏[J] .古地理学报, 2003 , 5(4):497-508 .
[5] 吴丽艳 , 陈春强 , 江春明 , 等 .浅谈我 国油气勘 探中的 古地貌 恢复技术[J] .石油天然气学报 , 2005 , 27(4):559-586 .
[6] 徐国强 , 李国蓉 , 刘树根 , 等 .塔里木 盆地早海 西期多 次风化 壳岩溶洞穴层[J] .地质学报 , 2005 , 79(4):557-568 .
[7] 代金友 , 史若珩 , 何顺利 .鄂尔多斯盆地中部 气田沟槽识别新 方法[J] .天然气工业 , 2006 , 26(4):26-28 .
[8] 王家豪 , 王 华 , 赵忠 新 , 等 .层 序 地层 学 应用 于 古地 貌分 析 ———以塔河油田为例[J] .地球 科学 ———中国 地质 大学学 报 , 2003 , 28(4):425-430 .
[9] 刘栓驹 , 黄 杰 , 王根久 , 等 .碳酸盐 岩潜山油 藏古地 貌及剩 余油分布关系[J] .石油学报 , 1999 , 20(2):39-44 .
[10] 丁晓琪 , 张哨 楠 , 王少飞 , 等 .鄂尔多斯盆地西 南缘镇泾油田 长 6-2 沉积相研究[J] .新疆地质 , 2007 , 25(1):105-110 .
[11] 周 瑞 , 胡学智 .鄂尔多 斯盆地西 北部灵盐 定地区油 藏类型 及其控制因素[J] .石油实验地质 , 2001 , 23(4):390-394 .
[12] 喻 建 , 宋江海 , 向 惠 .鄂尔多斯盆地中生界隐 蔽性油气藏 成藏规律[J] .天然气工业 , 2004 , 24(12):35-40 .
[13] 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] .地球科学与环境学报, 2003 , 25(4):9-12 .
[14] 郭正权 .前侏罗纪古地貌刻画技术[J] .低渗 透油气田 , 2001 , 6(3):64 .
[15] 郭正权 .鄂尔多斯盆地侏罗系古地貌油田的形成 条件与分布 规律[C] ∥杨 华 .低渗透油气田 研究与实 践 .北京 :石油工 业出版社 , 2001 :51-60 .
[16] Chi lingari an G V .Compact ion of C oarse-g rained S ediment s [M] .New York :E lsevier Scient ific Pub li sh , 1975 .
[17] 付 广 , 许泽剑 , 韩 冬玲 , 等 .不整 合面在油气藏形 成中的作 用[J] .大庆石油学院学报 , 2001 , 25(1):1-4 .
[18] 赵 卫军 , 支东明 , 党 玉芳 , 等 .准噶 尔盆地陆西地区 侏罗系西 山窑组顶界不整合结构特征及其与油气 关系[J] .新疆地质 , 2007 , 25(1):92-96 .

Memo

Memo:
-
Last Update: 2008-12-20