Abstract
AbstractIt has always been the focus of researchers to accurately identify gas hydrate location. Geophysical prospecting is a widely used method for gas hydrate exploration, which has high credibility, especially seismic exploration technology is most generally used. In our study, we analyze the different physical properties of gas hydrate and other minerals bearing in unconsolidated marine sediments based on the effective medium theory. Then, a new attribute is put forward to discriminate gas hydrate. The logging data in the Dongsha area of the South China Sea and the Hydrate Ridge along the Oregon continental margin are applied to validate this method. Our test results are basically in line with actual situation, which provides a new approach in hydrate identification.
Funder
Guangzhou Marine Geological survey
National Basic Research Program of China (973 Program)
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics,Oceanography
Reference35 articles.
1. Carcione JM, Tinivella U (2000) Bottom-simulating reflectors: seismic velocities and AVO effects. Geophysics 65(1):54–67
2. Chand S, Minshull TA, Gei D, Carcione JM (2004) Elastic velocity models for gas-hydrate-bearing sediments-a comparison. Geophys J Int 159:573–590. https://doi.org/10.1111/j.1365-246X.2004.02387.x
3. Collett TS, Knapp CC, Johnson AH, Boswell R (2009) Natural gas hydrate: a review. Am Assoc Pet Geol Mem, 89, 146–219. https://refhub.elsevier.com/S0264-8172(15)00170-1/sref7
4. Cook AE, Anderson BI, Malinverno A, Mrozewxki S, Goldberg DS (2010) Electrical anisotropy due to gas hydrate-filled fractures. Geophysics 75:173–185
5. Ecker C, Dvorkin J, Nur A (1998) Sediments with gas hydrates: internal structure from seismic AVO. Geophysics 63:1659–1669
Cited by
5 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献