Distributions and Applications of Nitrogen- and Oxygen-Containing Compounds in the Saline Lacustrine Source Rocks of the Baoding-Raoyang Sag, Bohai Bay Basin, Eastern China. [PDF]
Liu J, Li S, Li X.
europepmc +1 more source
Geochemistry of Totogan Formation as potential source rock and its relationship with oil seepage manifestations in the Banjarnegara areas, Central Java, Indonesia. [PDF]
Praptisih +6 more
europepmc +1 more source
Investigation of Hydrocarbon Generation from Jurassic Coal Measures in the Southern Junggar Basin, Northwestern China, Using Closed-System Pyrolysis. [PDF]
Gong D, Wang Q, Qi X, Liu G, Qin Z.
europepmc +1 more source
Characteristics of the Coal-Associated Shale and Its Paleoenvironmental Analysis of the Upper Triassic Tumengela Formation in the Central Part of the Qiangtang Basin. [PDF]
Peng Q +7 more
europepmc +1 more source
Investigating Pore Characteristics and Their Dependence on Shale Composition: Case Study from a Permian Basin in India. [PDF]
Ghosh Dastidar S +4 more
europepmc +1 more source
Multiscale Characterization and Mobility Evaluation of Storage Space in Laminated Shale Reservoirs: A Case Study of the Qingshankou Formation, Southern Songliao Basin. [PDF]
Wang H +8 more
europepmc +1 more source
Hydrocarbon generation potential in jurassic source rocks from hydrous pyrolysis experiments under ultradeep conditions. [PDF]
Cao Z, Liang M, Zhang X, Su L.
europepmc +1 more source
Organic Matter Enrichment in Jurassic Hydrocarbon Source Rocks from the Turpan-Hami Basin: Insights from Organic and Elemental Geochemistry. [PDF]
Liang H, Wang Z, Wang J, Wang X.
europepmc +1 more source
Comparative Rock-Eval pyrolysis as an improved tool for sedimentary organic matter analysis
An improved Rock-Eval pyrolysis method is described for the global and exhaustive characterization of kerogen and bitumen in rock samples. Comparative pyrolysis is derived from the original Rock-Eval method of Espitalie et al., it overcomes some of its inadequacies and allows a better exploitation of the pyrolysis data.
D. Delvaux +3 more
exaly +3 more sources

