Natural Gas Geoscience

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The sandstone characteristics and hydrocarbon exploration signification of Lower Jurassic in middle east section of northern tectonic belt in Kuqa Depression, Tarim Basin

Rong-hu Zhang, Hai-jun Yang, Hong-xing Wei, Chao-feng Yu, Zhao Yang, Jin Wu

Natural Gas Geoscience, 2019, 30(9): 1243-1252. DOI: 10.11764/j.issn.1672-1926.2019.05.005

Fig.10 Jurassic accumulation model in the Dibei slope belt-Tugeerming uplift belt, middle-east section of northern tectonic belt of Kuqa Depression

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Fig.1 Geological characteristics of the Lower Jurassic in the middle east section of the northern tectonic belt of Kuqa Depression
Fig.2 Sedimentary facies model of Middle and Lower Jurassic (Ahe-Yangxia-Kezilenur Formations)
Fig.3 Plan of sedimentary facies of Lower Jurassic Ahe Formation in the eastern part of Kuqa Depression in the northern tectonic belt of Kuqa Depression
Fig.4 Plan of sedimentary facies of Lower Jurassic Yangxia Formation in the eastern part of Kuqa Depression
Fig.5 Plan of sedimentary facies of Middle Jurassic Kezilenur Formation in the eastern part of Kuqa Depression
Fig.6 Sedimentary sand body and its configuration map of Lower Jurassic Ahe Formation in the middle section (Kuqa river area) of the northern tectonic belt of Kuqa Depression
Fig.7 Sedimentary sand body correlation and configuration diagram in the middle and lower part of Jurassic Yangxia Formation in the middle eastern section of northern tectonic belt of Kuqa Depression
Fig.8 Characteristics of upper sand body of Jurassic Kezilenur Formation in Tugeerming area,northern tectonic belt of Kuqa Depression
Fig.9 Jurassic hydrocarbon accumulation model in the east-west direction of Tugeerming anticline in the northern tectonic belt of Kuqa Depression
Fig.11 Reservoir correlation map of Jurassic Ahe Formation in the middle part (Kuqa river-Dibei slope belt) of northern tectonic belt of Kuqa Depression

模态框（Modal）标题

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