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Journal Article

Wide-Azimuth, Broadband, and High-Density Seismic Technology and Its Application for Prediction of Residual Oil Distribution

G. Aliyeva, X.D. Wei, Y. Liu, Q.H. Nie, J.X. Dong, X. Chen, X.H. Yan, K. Yang, A.S. Hakro, J.N. Tian
Published: 01 April 2023
Russ. Geol. Geophys. (2023) 64 (4): 495–509.
DOI: https://doi.org/10.2113/RGG20224489
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Journal Article

Integrating the Geology, Seismic Attributes, and Production of Reservoirs to Adjust Interwell Areas

A.K. Zhumabekov, Z. Liu, V.S. Portnov, X. Wei, X. Chen
Published: 01 July 2022
Russ. Geol. Geophys. (2022) 63 (7): 856–868.
DOI: https://doi.org/10.2113/RGG20214343
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Journal Article

Rates of subcritical cracking and long-term rock erosion

M.C. Eppes, G. S. Hancock, X. Chen, J. Arey, T. Dewers, J. Huettenmoser, S. Kiessling, F. Moser, N. Tannu, B. Weiserbs, J. Whitten
Journal: Geology
Published: 25 September 2018
Geology (2018) 46 (11): 951–954.
DOI: https://doi.org/10.1130/G45256.1
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Journal Article

Pridoli graptolites from northern Xinjiang, Northwest China

Y -n Ni, A C Lenz, X Chen
Published: 01 October 1998
Canadian Journal of Earth Sciences (1998) 35 (10): 1123–1133.
DOI: https://doi.org/10.1139/e98-059
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Book Chapter

Geostatistical Methods for the Study of Pressure Compartments: A Case Study in the Hilight Oil Field, Powder River Basin, Wyoming

Author(s)
X. Chen, L. Borgman, H. P. Heasler
Book: Basin Compartments and Seals
Series: AAPG Memoir
Publisher: American Association of Petroleum Geologists
Published: 01 January 1994
DOI: 10.1306/M61588C17
EISBN: 9781629810935
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Abstract This chapter introduces the variogram method for analyzing the geometry of pressure compartments. Pressure and hydraulic head data from 192 wells in the Hilight oil field, Powder River basin, Wyoming, were used in this study. Variograms were calculated for various directions. Results indicate that hydraulic head and pressure are spatially correlated, especially in directions parallel to the axes of elongation of compartment cells. The average pressure compartment was estimated via the variogram method to be an ellipse with major and minor axes of 5.3 and 2.7 mi (8.5 and 4.3 km). The major axis trends 15° azimuthally, the minor axis 285°.