2015 GSA Annual Meeting in Baltimore, Maryland, USA (1-4 November 2015)

Paper No. 120-27
Presentation Time: 9:00 AM-6:30 PM

STRATIGRAPHIC ANALYSIS AND GEOACOUSTIC MODELLING AT THE DH-1, 2 LONG-CORE SITES IN THE KOREAN CONTINENTAL MARGIN OF THE EAST SEA


RYANG, Woo Hun, Division of Science Education, Chonbuk National University, College of Education, Jeonju 561-756, Jeonju, Jeonbuk, 561-756, South Korea and KIM, Seong Pil, Divsion of Petroleum and Submarine Resources, Korea Institute of Geoscience and Mining Resources, Daejeon, 305-350, South Korea, ryang@jbnu.ac.kr

In the Korean continental margin of the western East Sea, stratigraphic and bottom models were investigated on the basis of long-core data and stratigraphic analysis with subbottom and air-gun profiles in the core sites. The long cores of 23.6 m and 27.2 m were acquired at the DH-1, 2 sites where are located near the Donghae City and the water depths are 357.8 m and 316.6 m deep, respectively. The long-core sediments were recovered using the Portable Remotely Operated Drill (PROD), a fully contained drilling system, remotely operated at the seafloor. The recovered core sediments were analyzed for physical, sedimentological, and geoacoustic properties mostly at 10~30 cm intervals. The detailed geoacoustic model at the DH-1 core site comprises vertical data of the 125 P-wave speeds and 121 P-wave attenuations of 23.6 m core sediments, consisting of 7 geoacoustic units. The geoacoustic model of the DH-2 core site was based on vertical measurements of the 86 P-wave speeds and 76 attenuation values of 27.2 m core sediments. These stratigraphic and geoacoustic models probably contribute for understanding vertical and lateral variability of acoustic properties in the Korean continental margin of the western East Sea.

Acknowledgements: This research was supported by Basic Science Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Education, Science and Technology (2010-0025733) and by the Ministry of Trade, Industry, and Energy through the grant of Marine Geology and Geophysical Mapping Project (GP2010-013).