中国石油勘探 ›› 2016, Vol. 21 ›› Issue (3): 38-51.

• 勘探案例 • 上一篇    下一篇

塔里木盆地顺托果勒隆起奥陶系碳酸盐岩超深层油气突破及其意义

漆立新   

  1. 中国石化西北油田分公司
  • 出版日期:2016-05-15 发布日期:2016-05-15
  • 基金资助:
    国家科技重大专项“塔里木—鄂尔多斯盆地海相碳酸盐岩层系大中型油气田形成规律与勘探评价”(2011ZX05005-004),“塔里木盆地碎屑岩系大型油气田富集规律与勘探方向”(2011ZXC05002-003)。

Oil and gas breakthrough in ultra-deep Ordovician carbonate formations in Shuntuoguole uplift, Tarim Basin

Qi Lixin   

  1. Sinopec Northwest Oilfield Company
  • Online:2016-05-15 Published:2016-05-15

摘要: 塔里木盆地顺托果勒隆起形成于加里东中期,早寒武世早期发育玉尔吐斯组斜坡—陆棚相烃源岩,早寒武世—中奥陶世发育了厚达3000m的碳酸盐岩沉积建造,多期海平面变化有利于形成暴露溶蚀型储层,同时加里东—海西期多期断裂发育,有利于裂缝发育和流体改造形成多类型储层,晚奥陶世沉积的巨厚泥岩可以作为区域盖层。该隆起下古生界发育完整的生储盖组合,是油气成藏有利地区。前期油气勘探主要集中在沙雅隆起与卡塔克隆起区,对深埋的顺托果勒隆起认识不足。通过深化基础研究,认识到顺托果勒隆起长期处于低地温背景,下寒武统烃源岩在喜马拉雅期仍处于凝析油—天然气生成阶段,具备形成晚期成藏的大型油气田的有利条件,寒武系—中下奥陶统碳酸盐岩是最主要的目的层系。在沙漠地区超深层地震技术攻关基础上优选目标实施钻探,取得了重大突破,勾勒出顺托果勒隆起大油气田的轮廓,有望实现塔中—塔北连片含油气格局。

关键词: 塔里木盆地, 顺托果勒隆起, 奥陶系, 碳酸盐岩, 超深层, 油气突破

Abstract: The Shuntuoguole uplift in the Tarim Basin was formed in the middle stage of Caledonian. In the early stage of Early Cambrian, the Yuertusi Formation slope-shelf facies source rocks were formed. During the Early Cambrian-Middle Ordovician, carbonate sedimentary formations with thickness up to 3000 m were developed, and multiphase sea level fluctuation contributed to the formation of exposed karst reservoirs. Meanwhile, during the Caledonian-Hercynian, multiphase faulting activities occurred, which were favorable for fracture development and fluid reformation to form multiple types of reservoirs. The very thick mudstones deposited during the Late Ordovician can act as regional cap rocks. In the Shuntuoguole uplift, a complete source-reservoir-cap-rock assemblage exists in the Lower Palaeozoic, suggesting it a prospect of hydrocarbon accumulation. The oil and gas exploration at the earlier stage focused on the Shaya and Katake uplifts, while the deeply-buried Shuntuoguole uplift was not thoroughly understood. Further basic studies reveal that the Shuntuoguole uplift is in the low geothermal environment for a long term. During the Himalayan, the Lower Cambrian source rocks were generating condensate oil-natural gas, implying the favorable conditions for the formation of large oil and gas fields with late-stage accumulation. The Cambrian – Middle-Lower Ordovician carbonate rocks are the most important targets. Based on the seismic technology R&D for ultra-deep zones in desert areas, targets were selected for well drilling. Great breakthrough has been made. A giant oil and gas field in the Shuntuoguole uplift is taking shape. It is promising to realize a continuous oil and gas pattern in central and northern Tarim Basin.

Key words: Tarim Basin, Shuntuoguole uplift, Ordovician, carbonate rock, ultra-deep formation, oil and gas breakthrough