Citation: | WANG Junzhu, QIN Chuqian, LUO Xulong, WANG Shidong, YANG Nan. APPLICATION PROSPECT OF CPT IN GAS HYDRATE EXPLORATION[J]. Marine Geology Frontiers, 2019, 35(11): 52-59. doi: 10.16028/j.1009-2722.2019.11008 |
Geophysical, geochemical, microbial and geological methods are widely used in gas hydrate exploration and 3D seismic method is doubtlessly the main and most important one. There are obvious differences in physical properties of sediments containing free natural gas and gas hydrates. The distribution of gas hydrates can be recognized by using these differences with 3D seismic data. However, some sediments, such as carbonate rocks may produce similar anomalies. CPT has prominent advantages in accurately determining the physical properties and types of sediments. It has the capability to carry out tasks such as soil mechanics testing, soil photography taking, geological sampling, P-S logging, thermodynamic testing, magnetic observation, conductivity testing, radioisotope testing and chemical analysis testing, etc. Combined with other methods, CPT is believed a very promising method for accurately determinating hydrate distribution and calculating gas reserves in gas hydrate exploration.
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Collocated CPT measurements, grain size distributions from sieving analysis and estimated grain size distributions based on CPT measurements at Krauthausen test site
Bathymetry map showing: the gravity cores locations (KS) the CPTU (PM) and Sonic CPT (PV) measurements positions (modified from reference[32])
Compressional wave velocity as a function of depth obtained from in-situ Sonic CPT measurements compared to Vp values obtained from the 1st reflector (for the upper 15 m) of the 3D seismic data at site
Pore pressure as a function of depth of the site bearing gas hydrates (modified from reference [32])