A study of velocity and attenuation anisotropy characteristics of turbidite thin interbed saturated with fluid: A case study of Beihai turbidite
TANG Jie1,2, WANG Hao1,2, LI Jian1,2, SU Wen-Han1,2, YAO Zhen-An1,2
1. School of Geosciences, China University of Petroleum, Qingdao 266580, China;
2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
In this paper,the authors studied velocity and attenuation anisotropy characteristics of turbidite thin interbed saturated with fluid,and analyzed the main influence factors such as group angle,net-to-gross,saturation and porosity.The results show that there are differences in condition between low frequency and high frequency.Through the anisotropy velocity analysis,the authors detected that compressional wave velocity increases with the increase of saturation and angle,and compressional wave velocity decreases with the increase of the net to gross.Through the attenuation anisotropy analysis,it's known that compressional wave attenuation parallel to the bedding is less than the result perpendicular to the bedding plane.Attenuation depends on the medium heterogeneity,and when medium inhomogeneity is maximum,attenuation is the largest.
唐杰, 王浩, 李健, 苏文涵, 姚振岸. 含流体浊积岩速度与衰减各向异性特征研究——以北海浊积岩为例[J]. 物探与化探, 2017, 41(1): 153-157.
TANG Jie, WANG Hao, LI Jian, SU Wen-Han, YAO Zhen-An. A study of velocity and attenuation anisotropy characteristics of turbidite thin interbed saturated with fluid: A case study of Beihai turbidite. Geophysical and Geochemical Exploration, 2017, 41(1): 153-157.