TitleMethods for Shale Gas Play Assessment: A Comparison between Silurian Longmaxi Shale and Mississippian Barnett Shale
AuthorsPan, Songqi
Zou, Caineng
Yang, Zhi
Dong, Dazhong
Wang, Yuman
Wang, Shufang
Wu, Songtao
Huang, Jinliang
Liu, Qun
Wang, Dule
Wang, Ziyuan
AffiliationPeking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China.
PetroChina, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China.
Southwest Petr Univ, Chengdu 610500, Peoples R China.
Keywordsshale gas play
Silurian Longmaxi shale
Barnett shale
sweet spot
six-property assessment
FORT-WORTH BASIN
TOTAL PETROLEUM SYSTEM
NORTH-CENTRAL TEXAS
SICHUAN BASIN
CHINA
ACCUMULATION
RESERVOIR
HYDROCARBON
MECHANISMS
GEOLOGY
Issue Date2015
Publisherjournal of earth science
CitationJOURNAL OF EARTH SCIENCE.2015,26,(2),285-294.
AbstractBased on field work, organic geochemical analyses and experimental testing, a six-property assessment method for shale gas is proposed. These six properties include organic matter properies, lithofacies, petrophysical properties, gas content, brittleness and local stress field. Due to the features of continuous distribution over a large area and low resource abundance in shale plays, a sweet spot should have these following properties: (a) TOC>2%; (b) brittle minerals content (>40%) and clay minerals (<30%); (c) Ro (>1.1%); (d) porosity (>2%) and permeability (>0.000 1 mD), and (e) effective thickness (30-50 m). Applying these criteria in the Sichuan Basin, the Silurian Longmaxi shale consists of four prospecting sweet spots, including blocks of Changning, Weiyuan, Zhaotong and Fushun-Yongchuan. Although these four blocks have some similarities, different features were usually observed. After comprehensive analyses using the six-property assessment method, the Fushun-Yongan Block ranks the most favorable sweet spot, followed by the Weiyuan Block. For the other two blocks, the Changning Block is better than the Zhaotong Block. By comparing with the Mississippian Barnett shale, characteristics that are crucial for a high-yielding in the Sichuan Basin include a high content of organic matter (TOC>2.5%), a moderate thermal maturity (Ro=0.4%-2%), a high content of brittle minerals (quartz: 30%-45%), a high gas content (>2.5 m(3).t(-1)), and types I and II1 kerogen.
URIhttp://hdl.handle.net/20.500.11897/155315
ISSN1674-487X
DOI10.1007/s12583-015-0524-0
IndexedSCI(E)
中国科学引文数据库(CSCD)
Appears in Collections:地球与空间科学学院

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