首页> 外文期刊>Journal of Petroleum Exploration and Production Technology >Geochemical evaluation of shale formations in the northern Song Hong basin, Vietnam
【24h】

Geochemical evaluation of shale formations in the northern Song Hong basin, Vietnam

机译:越南宋红盆地北部页岩形成的地球化学评价

获取原文
           

摘要

Petroleum exploration and production of conventional reservoirs have been strongly developed over the years in Vietnam since 1987. However, with the decrease in petroleum production in recent years, a certain attention has started to be given to the unconventional reservoirs. This study presents the results of a comprehensive geochemical evaluation of three main shale formations in the northern Song Hong basin (also known as the Red River basin) of Vietnam. Over 200 cutting samples of Lower Miocene, Oligocene and Triassic shales from two onshore and two offshore wells were collected and tested for total organic carbon (TOC), hydrocarbon generation potential (S2), hydrogen index (HI), production index (PI), Tmax and vitrinite reflectance (Ro). Lower Miocene shales are characterized by HI of 94 to 591 mgHC/gTOC, TOC of 0.14 to 1.65?wt% and S2 of 0.34 to 4.62?mg?HC/g?rock, indicating a poor-to-fair source rock of mixed gas-prone kerogen types II and III. Their Tmax of 425 to 437?°C and Ro of 0.35 to 0.66% suggested an immaturity to early-maturity HC generation. Oligocene shales have HI of 164 to 602?mgHC/gTOC, TOC of 0.52 to 3.18?wt% and S2 of 0.63 to 5.61?mg?HC/g?rock, indicating a fair-to-good potential source rock with a gas- and oil-prone kerogen of mixed types II and III. Their Tmax values of 427 to 476?°C and Ro of 0.43 to 1.73% suggested an optimum thermal maturity. Triassic shales are characterized by HI
机译:自1987年以来,越南多年来一直在大力开发和开发常规油藏。但是,随着近年来石油产量的下降,已经开始对非常规油藏给予一定的关注。这项研究提出了对越南北部宋洪盆地(也称为红河流域)北部三个主要页岩地层进行综合地球化学评估的结果。从两个陆上和两个海上井中收集了200多个下中新世,渐新世和三叠纪页岩的采掘样品,并测试了总有机碳(TOC),烃生成潜力(S2),氢指数(HI),生产指数(PI), Tmax和镜质体反射率(Ro)。下中新世页岩的特征是HI为94至591 mgHC / gTOC,TOC为0.14至1.65?wt%,S2为0.34至4.62?mg?HC / g?岩石,表明混合气来源较不公平II型和III型容易产生的干酪根。它们的Tmax为425至437°C,Ro为0.35至0.66%,表明HC生成尚不成熟。渐新世页岩的HI为164至602?mgHC / gTOC,TOC为0.52至3.18?wt%,S2为0.63至5.61?mg?HC / g?以及II型和III型混合的易生油干酪根。它们的Tmax值为427至476°C,Ro为0.43至1.73%,表明最佳的热成熟度。三叠纪页岩的特征是HI <?50?mgHC / gTOC,TOC为1.04至14.10 wt%和S2为0.03至1.11?mg?HC / g?岩石,显示出几乎没有残留源或在后期至后期没有生烃的潜力。成熟后阶段的Ro为1.79至2.10%。这项研究的新获得的地球化学数据和分析结果有望改善对宋洪盆地北部特别是陆上部分主要烃源岩的认识,并为进一步评估页岩气潜力提供有用的背景信息。在越南。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号