[1]韩长城,林承焰,鲁新便,等.塔河油田奥陶系岩溶地貌对储集层的控制作用[J].新疆石油地质,2016,(04):417.[doi:10.7657/XJPG20160406]
 HAN Changcheng,LIN Chengyan,LU Xinbian,et al.Controlling Effects of Ordovician Karst Paleogeomorphology on Reservoirs in Tahe Oilfield,Tarim Basin[J].Xinjiang Petroleum Geology,2016,(04):417.[doi:10.7657/XJPG20160406]
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塔河油田奥陶系岩溶地貌对储集层的控制作用()
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《新疆石油地质》[ISSN:1001-3873/CN:65-1107/TE]

卷:
期数:
2016年04期
页码:
417
栏目:
出版日期:
2016-08-01

文章信息/Info

Title:
Controlling Effects of Ordovician Karst Paleogeomorphology on Reservoirs in Tahe Oilfield,Tarim Basin
文章编号:
1001-3873(2016)04-0417-06
作者:
韩长城1林承焰1鲁新便2魏婷3任丽华1张宪国1
(1.中国石油大学 地球科学与技术学院,山东 青岛 266580;2.中国石化 西北油田分公司,乌鲁木齐 830011;3.中国石油 新疆油田分公司 石西油田作业区,新疆 克拉玛依 834000)
Author(s):
HAN Changcheng1 LIN Chengyan1 LU Xinbian2 WEI Ting3 REN Lihua1 ZHANG Xianguo1
(1.School of Geosciences, China University of Petroleum, Qingdao, Shandong 266580, China; 2.Northwest Oilfield Company,Sinopec, Urumqi, Xinjiang 830011, China; 3.Shixi Oilfield Operation District, Xinjiang Oilfield Company, PetroChina,Karamay, Xinjiang 834000, China)
关键词:
塔里木盆地塔河油田奥陶系古地貌岩溶储集层印模法残差厚度法地貌单元
Keywords:
Tarim basin Tahe oilfield Ordovician paleogeomorphology karst reservoir impression method residualthickness methodpaleogeomorphic unit
分类号:
TE112.221
DOI:
10.7657/XJPG20160406
文献标志码:
A
摘要:
综合利用大量岩心、薄片,钻井、测井、地震等资料,对古岩溶识别标志进行了分析;运用印模法、残差厚度法和不整合类型相结合,恢复了奥陶系岩溶古地貌,对古地貌单元进行划分并分析其对储集层的控制作用。在岩溶高地、岩溶缓坡、岩溶陡坡和岩溶盆地4个二级地貌单元,分别定量划分出残丘、台地、阶坪和沟谷4个三级地貌单元。岩溶缓坡区残丘、台地、沟谷末端、沟谷两侧及岩溶陡坡区台地和阶坪是岩溶储集层发育的有利区。
Abstract:
Using the data of core, thin section, drilling, logging and seismic profile, the mark of palaeokarst identification is analyzed; the Ordovician karst palaeogeomorphology is restored with impression method and residual thickness method combined with unconformity structures; karst paleogeomorphic units are classified and their controlling effects on reservoirs are analyzed. In the 4 secondary paleogeomorphic units such as karst highland, karst gentle?slope, karst steep?slope and karst basin, 4 tertiary paleogeomorphic units (monadnock, tableland, level terrace and clough) are further classified quantitatively. The favorable areas for karst reservoir development are monadnocks and tablelands in the karst gentle?slope, the ends and flanks of the clough, and the tablelands and level terraces in the karst steep?slope

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更新日期/Last Update: 2016-07-28