超高分辨率三维地震数据在墨西哥湾中斜坡深度地质灾害识别中的适用性:初步结果

IF 0.4 Q4 Engineering
B. Brookshire, Frank P Landers, J. Stein
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引用次数: 19

摘要

在墨西哥湾北部沿中斜坡深度收集的数据的初步结果表明,短偏移、超高分辨率、三维(UHR3D)地震方法在地质灾害探测和圈定中的适用性非常有希望。P-Cable™系统由18根长度为100米的拖缆和一支210英寸的3型发生器-喷射器(GI)气枪组成,在谐波模式下发射,实现了在海底下超过2s的双向行程时间(TWT)穿透。超过17°的倾角在海底下大于1s TWT处成像。在海底至海底以下1s TWT之间,恢复的主导频率约在78Hz ~ 100Hz之间。表观地下水平分辨率约为16m,地下垂直分辨率高达1.6m。海底分辨率与自然桶尺寸3.125 × 6.25m一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Applicability of ultra-high-resolution 3D seismic data for geohazard identification at mid-slope depths in the Gulf of Mexico: Initial results
Preliminary results from data collected along mid-slope depths in the northern Gulf of Mexico are very promising in regard to the applicability of short offset, ultra-high-resolution, three-dimensional (UHR3D) seismic methods in the detection and delineation of geohazards. Penetration of greater than 2s two-way travel time (TWT) below seabed was achieved with a P-Cable™ system comprising 18 streamers that were 100m in length and a 210in 3 Generator-Injector (GI) air gun fired in harmonic mode. Dips in excess of 17° were imaged at greater than 1s TWT below the sea floor. Between the sea floor and 1s TWT below the sea floor, the dominant frequency recovered is between about 78Hz and 100Hz. Apparent subsurface horizontal resolution is in the order of 16m, and subsurface vertical resolution is as high as 1.6m. Seafloor resolution is consistent with the natural bin size of 3.125 × 6.25m.
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来源期刊
UNDERWATER TECHNOLOGY
UNDERWATER TECHNOLOGY ENGINEERING, OCEAN-
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