Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.jngse.2019.01.022 |
Late Jurassic Arwa Member in south-eastern Al-Jawf sub-basin, NW Sabatayn Basin of Yemen: Geochemistry and basin modeling reveal shale-gas potential | |
Hakimi, Mohammed Hail1; Alaug, Abdulwahab S.1; Mohialdeen, Ibrahim M. J.2; Kahal, Ali Y.3; Abdulelah, Hesham4; Hadad, Yousif Taha5; Yahya, Madyan M. A.1,3 | |
通讯作者 | Hakimi, Mohammed Hail |
来源期刊 | JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING
![]() |
ISSN | 1875-5100 |
EISSN | 2212-3865 |
出版年 | 2019 |
卷号 | 64页码:133-151 |
英文摘要 | The current study evaluated the source rock characteristics, thickness, and lithology of the Late Jurassic Arwa Member to provide information about both conventional and unconventional resource systems in the Al-Jawf sub-basin. Three exploratory wells in the south-eastern portion of the Al-Jawf sub-basin were used for the source rock geochemistry and basin modeling study. Results from the geochemical and basin modeling indicate that the Arwa Member is a self contained source-reservoir whose shales are considered as gas-prone source rocks, and have generated large amounts of thermogenic gas through secondary cracking of oils at high thermal maturity levels. The geochemical results reveal that the Arwa shales currently contain Type III and IV kerogen in a gas-window maturity stage and are shale-gas resources. The basin models illustrate that the late Jurassic to early Miocene age was the peak-oil generation window of the Arwa shale source rock, with a transformation ratio (FR) of 10-85%. Most of the oil was expelled along micro-fractures caused by the pressure of oil generated within the Arwa shales, which was then trapped in the carbonate reservoir rocks within the Arwa Member itself. The oil retained in the Arwa carbonate rocks was partially and/or completely cracked into gas between the early Miocene and the present-day. This thermogenic gas was generated due to high thermal maturity caused by Tertiary volcanic rocks. Assuming a thickness of 360-1590 m and partial and/or complete cracking of retained oil to gas, the Arwa Shale Member could have a huge gas-generation potential. |
英文关键词 | Arwa shale Shale gas-potential Secondary cracking Geochemistry Basin modeling Al-Jawf sub-basin Yemen |
类型 | Article |
语种 | 英语 |
国家 | Yemen ; Iraq ; Saudi Arabia ; Malaysia ; Sudan |
收录类别 | SCI-E |
WOS记录号 | WOS:000460316000011 |
WOS关键词 | MARIB-SHABOWAH BASIN ; THERMAL MATURITY HISTORY ; NORTHERN WESTERN DESERT ; ORGANIC-RICH SHALES ; SOURCE-ROCK ; HYDROCARBON GENERATION ; SEDIMENTARY BASINS ; SHOUSHAN BASIN ; RED-SEA ; OIL |
WOS类目 | Energy & Fuels ; Engineering, Chemical |
WOS研究方向 | Energy & Fuels ; Engineering |
来源机构 | King Saud University |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/217250 |
作者单位 | 1.Taiz Univ, Fac Sci Appl, Dept Geol, Taizi 6803, Yemen; 2.Univ Sulaimani, Dept Geol, Coll Sci, Kurdistan, Iraq; 3.King Saud Univ, Dept Geol & Geophys, Coll Sci, Riyadh, Saudi Arabia; 4.Univ Teknol PETRONAS, Fac Petr & Geosci, Inst Hydrocarbon Recovery, SGRG, Seri Iskandar 32610, Malaysia; 5.OEPA, Minist Petr, HQ, Khartoum, Sudan |
推荐引用方式 GB/T 7714 | Hakimi, Mohammed Hail,Alaug, Abdulwahab S.,Mohialdeen, Ibrahim M. J.,et al. Late Jurassic Arwa Member in south-eastern Al-Jawf sub-basin, NW Sabatayn Basin of Yemen: Geochemistry and basin modeling reveal shale-gas potential[J]. King Saud University,2019,64:133-151. |
APA | Hakimi, Mohammed Hail.,Alaug, Abdulwahab S..,Mohialdeen, Ibrahim M. J..,Kahal, Ali Y..,Abdulelah, Hesham.,...&Yahya, Madyan M. A..(2019).Late Jurassic Arwa Member in south-eastern Al-Jawf sub-basin, NW Sabatayn Basin of Yemen: Geochemistry and basin modeling reveal shale-gas potential.JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING,64,133-151. |
MLA | Hakimi, Mohammed Hail,et al."Late Jurassic Arwa Member in south-eastern Al-Jawf sub-basin, NW Sabatayn Basin of Yemen: Geochemistry and basin modeling reveal shale-gas potential".JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING 64(2019):133-151. |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。