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Volume 103, Number 7
July 2019
AAPG Bulletin Cover Image for Volume 103, Issue 7
ISSN: 0149-1423
EISSN: 1558-9153
In this Issue

ARTICLES

Detrital zircon ages: A key to unraveling provenance variations in the eastern Yinggehai–Song Hong Basin, South China Sea
Ce Wang; Xinquan Liang; David A. Foster; Xirong Liang; Chuanxin Tong; Ping Liu
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Generation and evolution of overpressure caused by hydrocarbon generation in the Jurassic source rocks of the central Junggar Basin, northwestern China
Xiaowen Guo; Sheng He; Keyu Liu; Zhi Yang; Shengqiang Yuan; Mingliang Liu
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Architecture, geomorphology, and sediment gravity flows of a Jurassic subaqueous clinoform system, northeast Exmouth Plateau, North West Shelf, Australia
Peng Chen; Chris Elders
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Thermal properties of sedimentary rocks in the Tarim Basin, northwestern China
Xianglan Li; Shaowen Liu; Changge Feng
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Charging of Carboniferous volcanic reservoirs in the eastern Chepaizi uplift, Junggar Basin (northwestern China) constrained by oil geochemistry and fluid inclusion
Xiangchun Chang; Yue Wang; Bingbing Shi; Youde Xu
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Sequence stratigraphy and coal accumulation of Lower Cretaceous coal-bearing series in Erlian Basin, northeastern China
Shuai Wang; Longyi Shao; Dongdong Wang; Qinping Sun; Bin Sun; Jing Lu
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From trash to treasure: Three-dimensional basement imaging with “excess” data from oil and gas explorations
Doyeon Kim; Larry D. Brown
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Formation and preservation of a giant petroleum accumulation in superdeep carbonate reservoirs in the southern Halahatang oil field area, Tarim Basin, China
Guangyou Zhu; Alexei V. Milkov; Zhiyao Zhang; Chonghao Sun; Xiaoxiao Zhou; Feiran Chen; Jianfa Han; Yongfeng Zhu
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Geochemical investigations of the Woodford–Chattanooga and Fayetteville Shales: Implications for genesis of the Mississippi Valley–type zinc–lead ores in the southern Ozark Region and hyd...
Bryan Bottoms; Adriana Potra; John R. Samuelsen; Stephen R. Schutter
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  • Cover Image

    Cover Image

    issue cover

    ON COVER – The outcrops in the Aksu area, northwestern margin of the Tarim Basin. This is the best place for field study because it holds the complete succession of Paleozoic strata. Dolomites with abundant pores and fractures were well developed and the Cambrian source rocks were well preserved. See related article by Zhu et al., p. 1703 of this issue of the Bulletin.

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  • Online ISSN 1558-9153
  • ISSN 0149-1423
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