[1]陈春勇,谭 强,张金风,等.吉木萨尔凹陷二叠系梧桐沟组一段沉积演化规律[J].新疆石油地质,2015,36(02):169.[doi:10.7657/XJPG20150208]
 CHEN Chunyong,TAN Qiang,ZHANG Jinfeng,et al.Sedimentary Evolution of theMember1of Permian Wutonggou Formation in Jimusaer Sag, Junggar Basin[J].Xinjiang Petroleum Geology,2015,36(02):169.[doi:10.7657/XJPG20150208]
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吉木萨尔凹陷二叠系梧桐沟组一段沉积演化规律()
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《新疆石油地质》[ISSN:1001-3873/CN:65-1107/TE]

卷:
36
期数:
2015年02期
页码:
169
栏目:
出版日期:
2015-04-30

文章信息/Info

Title:
Sedimentary Evolution of theMember1of Permian Wutonggou Formation in Jimusaer Sag, Junggar Basin
文章编号:
1001-3873(2015)02-0169-05
作者:
陈春勇1谭 强1张金风1王 菁1袁春林2a康永尚2a 2b
(1. 中国石油 新疆油田分公司 准东采油厂 ,新疆 阜康 831511;2.中国石油大学 a.地球科学学院;b.油气资源与探测国家重点实验室,北京 102249)
Author(s):
CHEN Chunyong1 TAN Qiang1 ZHANG Jinfeng1 WANG Jing1 YUAN Chunlin2a KANG Yongshang2a2b
(1.Zhundong Oil Production Factory, Xinjiang Oilfield Company, PetroChina, Fukang, Xinjiang831511, China;2.China University of Petroleum, a.College of Earth Sciences, b.State Key Laboratory of Petroleum Resources and Prospecting, Beijing102249, China)
关键词:
准噶尔盆地吉木萨尔凹陷梧桐沟组梧一段沉积相辫状河三角洲沉积演化
Keywords:
Junggar basin Jimusaer sag Wutonggou formation Wu1member sedimentary facies braided river delta sedimentary evolution
分类号:
TE112.221
DOI:
10.7657/XJPG20150208
文献标志码:
A
摘要:
上二叠统梧桐沟组是准噶尔盆地吉木萨尔凹陷重要的含油气层系之一,梧一段是主要产油层,为满足梧桐沟组深化勘探的需要,开展了吉木萨尔凹陷梧一段5个砂层组沉积相和梧一段沉积演化规律研究。研究结果表明:梧一段不同沉积期发育了多个继承性辫状河三角洲,首次识别出吉15井西和吉南辫状河三角洲以及北三台凸起西南坡和三台古隆起周边小规模扇三角洲;梧一段继承性辫状河三角洲随着水体的不断扩张,逐渐向远离沉积中心的凹陷边缘迁移,有利于岩性圈闭的形成,不同期次的辫状河三角洲之间向上呈退积叠置关系,下部砂层组的砂体主要分布在凹陷中心部位,上部砂层组的砂体主要分布于凹陷边缘部位。
Abstract:
The Wutonggou formation of Upper Permian is one of the important hydrocarbon sequences in Jimusaer sag of Junggar basin, and the Wu?1member is the main oil producing zone. In this paper, five sand layers and sedimentary evolution laws of the Wu?1 memberwere studied for the purpose of the requirements of deepening petroleum exploration. The results show that there are several inherited braided river deltas developed in different stages of Wu?1member episode, and Ji?15well west and Jinan inherited braided river deltas as well as Beisantai swell southwest slope and Santai paleo?uplift small?scale fan deltas are identified for the first time. Along with lake extension, the inherited braided river deltas of Wu?1member moved away from the sedimentary center, which were favorable for formation of lithologic traps surrounding Jimusaer sag. The inherited braided river deltas developed in different stages have the retrograding contact relations among them, and the sand bodies of the lower sand layers are distributed in the central of the sag, while the sand bodies of the upper sand layers are distributed around the sag margin

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更新日期/Last Update: 2015-08-26