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- W2352180819 abstract "Two wide-angle seismic profiles across the Yinggehai Basin indicated a low ve-locity layer (LVL) in sediments at depth between 3. 5-9 km. Velocity analyses ofmulti-channel seismic reflection data and well logging data confirmed the existence ofLVL. The upper boundary of the LVL is diachronous and varies in depth between 1. 5km and 5 km, mostly shallower towards the center of the basin. Involved strata includeparts of Quaternary to Tertiary in the center of the basin, but parts of Tertiary only tothe north and southeast of the basin. Several factors have contributed to the genesis ofLVL. The high accumulation rate and subsequent under-compaction of sediments weremain factors for the northern and southeastern portions of the basin, while the multi-ep-isodic fluid activity and related diapir process played important roles in the center of thebasin and raised the upper boundary of LVL over there." @default.
- W2352180819 created "2016-06-24" @default.
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- W2352180819 date "2001-01-01" @default.
- W2352180819 modified "2023-09-23" @default.
- W2352180819 title "CHARACTERISTICS AND GENESIS OF LOW VELOCITYLAYER IN YINGGEHAI BASIN，NW SOUTH CHINA SEA" @default.
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