Hydrochemical characteristics and genesis model of Yaoshuitan geothermal field in Huangzhong District, Xining City. [PDF]
Guangxiong Q +4 more
europepmc +1 more source
Study of the Pore Structure and Fractal Characteristics of the Leping Formation Shale in the Junlian Block, Southern Sichuan Basin. [PDF]
Liang S +5 more
europepmc +1 more source
Greenhouse Gas Emissions during Oil Shale Crushing and Its Main Controlling Factors: A Contrast Study of Oil Shale in Yaojie and Fushun Areas, China. [PDF]
Wang L +6 more
europepmc +1 more source
Characteristics of Pore Structure and the Evolution Process in Terrestrial Shale Reservoirs: A Case Study of the Shahejie Formation in Dongpu Depression, Bohai Bay Basin. [PDF]
Xu Y +10 more
europepmc +1 more source
Spatiotemporal evolution analysis of multiscale fracture dynamics in hydraulic shale stimulation via integrated acoustic emission and CT imaging. [PDF]
Wei X, Cai M, Kong C, Zhao D.
europepmc +1 more source
Lacustrine Shale Oil Enrichment and Mobility in the Lower Cretaceous Shahai Formation, Fuxin Basin (NE China): Integrated Inorganic-Organic Geochemical and Petrographic Evidence. [PDF]
Xiao F +10 more
europepmc +1 more source
Data-driven total organic carbon prediction using feature selection methods incorporated in an automated machine learning framework. [PDF]
Macêdo BDS +7 more
europepmc +1 more source
Uranium mining fuels evolution in deep groundwater microbiomes
Xiu W +21 more
europepmc +1 more source
Abstract Based on analysis of well and drilling data, cores, sediment grains and 3D seismic data, four types of turbidites–slope fan, channelized, laminated and sublacustrine fan turbidite–are identified in Members 1 and 2 of the Qingshankou Formation in northern Songliao Basin. The slope fan turbidite is located in Members 1 and 2 of the Qingshankou
Shun Zhang, Chaodong Wu
exaly +3 more sources
According to the core observation and log facies analysis, in the stage of the sand group V of the second section of Qingshankou formation, it mainly develop the delta of type IV which was proposed by Coleman and Wright and in Daqingzi region ,the delta can be classified into two subfacies : delta front and prodelta. The delta front can be divided into
Ming Zhang +4 more
core +3 more sources

