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作 者:CAO Chunhui TANG Qingyan ZHANG Mingjie LV Zonggang
机构地区:[1]School of Earth Sciences & Key Lab of Mineral Resources in Western China , Gansu Province, Lanzhou University,Lanzhou 730000 [2]Key Laboratory of Petroleum Resources, Gansu Province~Key Laboratory of Petroleum Resources Research, Institute ofGeology and Geophysics, Chinese Academy of Sciences, Lanzhou 730000 [3]Shu'nan Gas-mine Field, PetroChina Southwest Oil & Gas Field Branch Company, Luozhou 648000
出 处:《Acta Geologica Sinica(English Edition)》2015年第A01期375-377,共3页地质学报(英文版)
摘 要:1 Introduction Many high yield shale gas areas in the World are discovered carbon isotope reversals: Barnett, Fayetteville (Zumberge et al., 2012), Marcellus (Tilley et al., 2013), Haynesville (Ferwom et al., 2008), Albany shale gas (Gao et al., 2014), Utica shale gas (Xia et al., 1999; Xia et al., 2012; Xia et al., 2013), the Foothills (Tilley et al., 2011), Horn River (Tilley et al., 2013) and Ordos basin shale gas (Wang et al., 2015; Dai et al., 2005).1 Introduction Many high yield shale gas areas in the World are discovered carbon isotope reversals: Barnett, Fayetteville (Zumberge et al., 2012), Marcellus (Tilley et al., 2013), Haynesville (Ferwom et al., 2008), Albany shale gas (Gao et al., 2014), Utica shale gas (Xia et al., 1999; Xia et al., 2012; Xia et al., 2013), the Foothills (Tilley et al., 2011), Horn River (Tilley et al., 2013) and Ordos basin shale gas (Wang et al., 2015; Dai et al., 2005).
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