Evidence of Pore‐ and Fracture‐Filling Gas Hydrates from Geophysical Logs in Consolidated Rocks of the Muli Area, Qinghai–Tibetan Plateau Permafrost, China

Author:

Peng C.12ORCID,Zou C. C.12ORCID,Lu Z. Q.3,Yu C.Q.4,Liu A. Q.12,Tang Y. Y.12,Hu X. D.12,Zhang S. X.12,Wen H. J.5,Li Y. H.5,Wang W. C.5

Affiliation:

1. Key Laboratory of Geo‐detection (China University of Geosciences, Beijing), Ministry of Education Beijing China

2. School of Geophysics and Information TechnologyChina University of Geosciences Beijing China

3. Oil and Gas SurveyChina Geological Survey Beijing China

4. State Key Laboratory of Continental Tectonics and Dynamics, Institute of GeologyCAGS Beijing China

5. Qinghai No. 105 Coal Geological Exploration Team Xining China

Funder

Ministry of Education of the People's Republic of China

China Geological Survey

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference67 articles.

1. Possible link between weak bottom simulating reflections and gas hydrate systems in fractures and macropores of fine-grained sediments: Results from the Hikurangi Margin, New Zealand

2. A simple, effective‐medium model for water saturation in porous rocks

3. Effective‐medium resistivity models for calculating water saturation in shaly sands;Berg C. R.;The Log Analyst Journal,1996

4. Electrical conductance in a porous medium

5. Study of the gas hydrate stability zone in Muri coalfield, Qinghai province, China;Cao D. Y.;Journal of China University of Mining and Technology,2013

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