VARIATION OF DRILLING MUD GAS COMPONENTS AT 350~800 m INTERVAL OF No. 2 BOREHOLE OF SCIENTIFIC DRILLING FOR WENCHUAN SEISMIC FAULTED ZONE
LIU Shu-bo1,2, TANG Li-jun2, SUN Qing2, CEN Kuang1
1. College of Earth Science and Resources, China University of Geosciences, Beijing 100083, China;
2. National Research Center for Geoanalysis, Bei- jing 100037, China
Based on data of some gas components in drilling mud at 350~800 m interval of No. 2 borehole for WFSD and Richter earthquake magnitude ML≥3.5 catalog as well as lithologic character of cores from the faulted zone of Wenchuan earthquake, the authors investigated the relationships of anomalies of drilling mud de-gas gaseous components to tectonic environment and earthquake activity. The results show that the shattering of rocks is maximum at the interval of 660~680 m, the normalized values of various gases also show obvious positive and negative anomalies, and the intervals corresponding to the maximum and minimum values are places where aftershocks higher than the magnitude MS 3.0 frequently occur. The gas anomalies mostly occur in cracks in rocks, surface of fractures and faults.
刘舒波, 唐力君, 孙青, 岑况. 汶川地震断裂带科学钻探工程2号孔350~800 m井段的钻探泥浆气体组分变化[J]. 物探与化探, 2012, 36(1): 48-53.
LIU Shu-bo, TANG Li-jun, SUN Qing, CEN Kuang. VARIATION OF DRILLING MUD GAS COMPONENTS AT 350~800 m INTERVAL OF No. 2 BOREHOLE OF SCIENTIFIC DRILLING FOR WENCHUAN SEISMIC FAULTED ZONE. Geophysical and Geochemical Exploration, 2012, 36(1): 48-53.