scholarly journals Lithofacies distribution characteristics and its controlling factors of shale in Wufeng Formation-Member 1 of Longmaxi Formation in the Jiaoshiba area

2018 ◽  
Vol 3 (4) ◽  
pp. 306-319 ◽  
Author(s):  
Chao Wang ◽  
Baiqiao Zhang ◽  
Yongchao Lu ◽  
Zhiguo Shu ◽  
Yaqiu Lu ◽  
...  
2019 ◽  
Vol 30 (5) ◽  
pp. 879-892 ◽  
Author(s):  
Wenda Zhou ◽  
Shuyun Xie ◽  
Zhengyu Bao ◽  
Emmanuel John M. Carranza ◽  
Lei Lei ◽  
...  

2019 ◽  
Vol 128 ◽  
pp. 103886 ◽  
Author(s):  
Han Bao ◽  
Yong Zhai ◽  
Hengxing Lan ◽  
Keke Zhang ◽  
Qun Qi ◽  
...  

Geofluids ◽  
2020 ◽  
Vol 2020 ◽  
pp. 1-13 ◽  
Author(s):  
Kaiyuan Liu ◽  
Jian Xiong ◽  
Xi Zhang ◽  
Xiao Fan ◽  
Le Li

The rock physics experiments and fracture toughness tests of shales from the Lower Silurian Longmaxi Formation in the Sichuan Basin in China were carried out. Based on this, the calculation model of the fracture toughness was constructed, thus, the single well evaluation of the fracture toughness in shale formation would be obtained based on the well logging data, which can be used to summarize the spatial distribution characteristics of the fracture toughness in the shale formation. However, it is difficult to obtain transverse distribution characteristics of fracture toughness in shale formation based solely on the well logging data. Therefore, in order to investigate the spatial distribution of the fracture toughness, jointing well logging and seismic method could be adopted to quantitatively predict the fracture toughness in shale formation. The results show that fracture toughness of shales is sensitive to acoustic interval transit time and wave impedance. The prediction model of the fracture toughness of shales was constructed, which had a good prediction effect. The fracture toughness values of shales from the Upper Silurian Wufeng-Longmaxi Formation were larger, whereas those of shales from the Lower Silurian Wufeng-Longmaxi Formation were lower. The fracture toughness is mainly distributed in strips along the vertical direction while the distribution area is continuous in the lateral direction, indicating that it has obvious stratification characteristics.


2013 ◽  
Vol 773 ◽  
pp. 800-805
Author(s):  
Gui You Lv

This article is intended to identify interface symbols of sand groups by combining logging data with seismic data, and set correlation symbols of 8 sand groups in strata Nen 3 (H1) and Nen 4 (H2) of Nenjiang group. Characteristics of interior gyrations of those sand groups are analyzed according to core and logging data. Besides, sand group features of a single well are expected to be studied in this article. Upon the data and analysis, foundation information is provided for the research on sand distribution characteristics of Heidimiao oil layer and controlling factors of oil and water distribution.


2013 ◽  
Vol 448-453 ◽  
pp. 3757-3761
Author(s):  
Yan Ru Meng ◽  
Zeng Xue Li ◽  
Hai Yan Liu ◽  
Nan Jiang ◽  
Juan Liu

Distribution characteristics of coalbed methane in Huanghebei mining area were studied and influence of geological factors such as faults, lithology of coal seam roof and floor, magmatic activities, burial depth and upper bedrock thickness of coal seam and hydrogeological conditions on occurrence of coalbed methane were deeply discussed in this paper. Coalbed methane content of mining area increased gradually from southeast to northwest. Coalbed methane in deep well points of mining area is dominated by methane and that in shallow parts contained higher content of nitrogen.


2014 ◽  
Vol 909 ◽  
pp. 463-466
Author(s):  
Lei Gong ◽  
Shu Jun Guo ◽  
Shuai Gao ◽  
Xian Xian Tao ◽  
Jian Guo Huang

Using the data of cores, outcrops, thin sections and image logs, we analyzed the fracture distribution characteristics in the ultra-low permeability reservoirs of Anpeng oilfield. Then, we analyzed the main factors controlling the development of fractures. There are tectonic fractures and diagenetic fractures in the ultra-low permeability reservoirs. Tectonic fractures with high dip-angle are the main fracture type. Under the stresses resulting from horizontal tectonic compressions in the Early and Late Himalayan movements, three sets of tectonic fractures formed in the study area, i.e. E-W, NE-SW and NW-SE orientations. The E-W oriented fractures are developed better, then the NE-SW and NW-SE oriented fractures. The formation and distribution of these tectonic fractures are controlled by the tectonic stress field, lithology, porosity, permeability, layer thickness and structures. Under the same controlling factors, the origin types, occurrences and development characteristics of fractures in shallow-to mid-depth reservoirs are similar to that in the deep reservoirs. But fractures developed better in the deep reservoirs than that in the shallow-to mid-depth reservoirs.


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