Issues
Volume 102, Number 10
1 October 2018
ISSN 0149-1423
EISSN 1558-9153
In this Issue
ARTICLES
Quantitative sequence stratigraphy
AAPG Bulletin October 01, 2018, Vol.102, 1913-1939. doi:10.1306/02201817271
Pore structure and spontaneous imbibition characteristics of marine and continental shales in China
AAPG Bulletin October 01, 2018, Vol.102, 1941-1961. doi:10.1306/03291817297
Characterization of the natural fracture system of the Eagle Ford Formation (Val Verde County, Texas)
AAPG Bulletin October 01, 2018, Vol.102, 1963-1984. doi:10.1306/03151817323
Practical and efficient three-dimensional structural restoration using an adaptation of the GeoChron model
AAPG Bulletin October 01, 2018, Vol.102, 1985-2016. doi:10.1306/03291817191
Application of four-dimensional monitoring to understand reservoir heterogeneity controls on fluid flow during the development of a submarine channel system
AAPG Bulletin October 01, 2018, Vol.102, 2017-2044. doi:10.1306/0227181613317111
Southern Gulf of Mexico Wilcox source to sink: Investigating and predicting Paleogene Wilcox reservoirs in eastern Mexico deep-water areas
AAPG Bulletin October 01, 2018, Vol.102, 2045-2074. doi:10.1306/03291817263
Estimation of original kerogen type and hydrogen index using inorganic geochemical proxies: Implications for assessing shale gas potential in the Devonian Horn River Formation of western Canada
AAPG Bulletin October 01, 2018, Vol.102, 2075-2099. doi:10.1306/0329181524617100
Inferring total organic carbon and major element geochemical and mineralogical characteristics of shale core from hyperspectral imagery
AAPG Bulletin October 01, 2018, Vol.102, 2101-2121. doi:10.1306/03291817217
Discovery of the lower Cambrian high-quality source rocks and deep oil and gas exploration potential in the Tarim Basin, China
AAPG Bulletin October 01, 2018, Vol.102, 2123-2151. doi:10.1306/03141817183
-
Cover Image
Cover Image
ON COVER – The newly discovered highquality source rock from Cambrian Yuertusi Formation in the Aksu area, Tarim Basin, China. These rocks are black shales and typically have a total organic carbon content between 2% to 6%. The overlying Cambrian dolomites in association with a salt seal exhibit favorable geological conditions for large-scale hydrocarbon accumulation. A new set of deep exploration strata can, therefore, be developed, guiding future deep Cambrian hydrocarbon exploration in the Tarim Basin. See related article by Zhu et al., p. 2123, this issue of the Bulletin.
- PDF Icon PDF LinkFront Matter
- PDF Icon PDF LinkTable of Contents
- PDF Icon PDF LinkBack Matter
