High-resolution seismic studies of gas hydrates west of Svalbard

被引:40
作者
Posewang, J
Mienert, J
机构
[1] Univ Kiel, SFB 313, D-24118 Kiel, Germany
[2] Univ Tromso, Dept Geol, N-9037 Tromso, Norway
关键词
D O I
10.1007/s003670050102
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A strong bottom-simulating reflection (BSR) with high-amplitude variations is detectable in high-resolution reflection seismic profiles west of Svalbard. Above the BSR, anomalously high velocities up to 1840 m/s, calculated from high-frequency ocean-bottom hydrophone (HF-OBH) data, indicate the existence of gas-hydrated sediments. Below the BSR, a low-velocity layer, interpreted as gas-bearing sediments, shows thickness variations from 12 to 25 m. In addition, two other low-velocity layers clearly containing free gas are detected within the classic hydrate stability zone (HZ) where, a theoretical viewpoint, free gas cannot exist.
引用
收藏
页码:150 / 156
页数:7
相关论文
共 27 条
[1]   SEISMIC STUDIES OF A BOTTOM SIMULATING REFLECTION RELATED TO GAS HYDRATE BENEATH THE CONTINENTAL-MARGIN OF THE BEAUFORT SEA [J].
ANDREASSEN, K ;
HART, PE ;
GRANTZ, A .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1995, 100 (B7) :12659-12673
[2]  
Andreassen K., 1990, First Break, V8, P235, DOI DOI 10.3997/1365-2397.1990012
[3]  
Andreassen K., 1995, NORSK GEOLOGISK TIDS, V45, P10
[4]  
[Anonymous], 1993, US GEOLOGICAL SURVEY
[5]  
BANGS NLB, 1993, GEOLOGY, V21, P905, DOI 10.1130/0091-7613(1993)021<0905:FGATBO>2.3.CO
[6]  
2
[7]  
Boehm G., 1995, Bollettino di Geofisica Teorica ed Applicada, V37, P3
[8]  
CAMERLENGHI A, 1994, TERRA ANTARCTICA, V1, P154
[9]  
CRANE K, 1995, NORSK POLARINSTITUTT, V137, P32
[10]  
DIETRICH G, 1969, CONSEIL INT EXPLORAT