Relationship of gas hydrate concentration to porosity and reflection amplitude in a research well, Mackenzie Delta, Canada SCIE SCOPUS

Cited 8 time in WEB OF SCIENCE Cited 12 time in Scopus
Title
Relationship of gas hydrate concentration to porosity and reflection amplitude in a research well, Mackenzie Delta, Canada
Author(s)
Jin, YK; Lee, MW; Collett, TS
Publication Year
2002-04
Abstract
Well logs acquired at the Mallik 2L-38 gas hydrate research well, Mackenzie Delta, Canada, reveal a distinct trend showing that the resistivity of gas-hydrate-bearing sediment,, increases with increases in density porosities, This trend, opposite to the general trend of decrease in resistivity with porosity, implies that gas hydrates are more concentrated in the higher porosity. Using the Mallik 2L-38 well data, a proportional gas hydrate concentration (PGHC) model, which states that the gas hydrate concentration in the sediment's pore space is linearly proportional to porosity. is proposed for the general habitat of gas hydrate in sediments. Anomalous data (less than 6% of the total data) outside the dominant observed trend can be explained by local geological characteristics. The anomalous data analysis indicates that highly concentrated gas-hydrate-bearing layers would be expected where sediments have high proportions of gravel and coarse sand. Using the parameters in the PGHC model determined from resistivity-porosity logs, it is possible to qualitatively predict the degree of reflection amplitude variations in seismic profiles. Moderate-to-strong reflections are expected for the Mallik 2L-38 well. (C) 2002 Elsevier Science Ltd, All rights reserved.
ISSN
0264-8172
URI
https://sciwatch.kiost.ac.kr/handle/2020.kiost/5723
DOI
10.1016/S0264-8172(02)00011-9
Bibliographic Citation
MARINE AND PETROLEUM GEOLOGY, v.19, no.4, pp.407 - 415, 2002
Publisher
ELSEVIER SCI LTD
Keywords
gas hydrate concentration; porosity; seismic amplitude; Mallik 2L-38 well data
Type
Article
Language
English
Document Type
Article
Publisher
ELSEVIER SCI LTD
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