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- W640649769 abstract "Deep-water mound-shaped sediment packages on the northern slope of the Xisha carbonate platforms in the northern South China Sea were analyzed by integrating high-resolution multi-channel seismic and drilling data. The mounds are distributed in the Beijiao depression of the Qiongdongnan Basin within the T41-T40 seismic horizons, which correspond to the middle Miocene. Mound-shaped reflections were identified both in the NE-SW and NW-SE oriented seismic profiles. The mound shapes are most prominent in the center of the NW-SE oriented seismic profiles, and the undulating tops flatten out towards the NW and SE. Similar reflections are mostly asymmetric, with steeper eastern flanks in the NE-SW oriented seismic profiles, and they are mostly round in shape. The wave impedance from the inversion calculation is 6-8 x 10(6) kg/(m(2).s). It is much lower than that of the reef reservoir in the LH11-1 Reef Oilfield. Paleogeographic analysis shows that the Xisha uplift was dominated by tropical shallow carbonate platforms, while the Beijiao depression became a bathyal environment in the middle Miocene. Drilling data confirmed that the mound-shaped sediment packages are mainly composed of calcareous mudstone. Therefore, we infer that the mound-shaped sediment packages could be reef complexes or they were presumably built by combined gravity flow and bottom current. (C) 2015 Elsevier Ltd. All rights reserved." @default.
- W640649769 created "2016-06-24" @default.
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- W640649769 date "2015-12-01" @default.
- W640649769 modified "2023-10-16" @default.
- W640649769 title "Middle Miocene mound-shaped sediment packages on the slope of the Xisha carbonate platforms, South China Sea: Combined result of gravity flow and bottom current" @default.
- W640649769 cites W1964979970 @default.
- W640649769 cites W1967318561 @default.
- W640649769 cites W1968000221 @default.
- W640649769 cites W1969831920 @default.
- W640649769 cites W1972306362 @default.
- W640649769 cites W1978928221 @default.
- W640649769 cites W1980814581 @default.
- W640649769 cites W1982645341 @default.
- W640649769 cites W1986877120 @default.
- W640649769 cites W1988661126 @default.
- W640649769 cites W1992356157 @default.
- W640649769 cites W1992444350 @default.
- W640649769 cites W1998643369 @default.
- W640649769 cites W2000053397 @default.
- W640649769 cites W2001770705 @default.
- W640649769 cites W2002775898 @default.
- W640649769 cites W2007125209 @default.
- W640649769 cites W2008684278 @default.
- W640649769 cites W2010164667 @default.
- W640649769 cites W2014167742 @default.
- W640649769 cites W2016213881 @default.
- W640649769 cites W2029675956 @default.
- W640649769 cites W2030545755 @default.
- W640649769 cites W2030675100 @default.
- W640649769 cites W2031032107 @default.
- W640649769 cites W2032375832 @default.
- W640649769 cites W2039956748 @default.
- W640649769 cites W2042619450 @default.
- W640649769 cites W2043942893 @default.
- W640649769 cites W2044668883 @default.
- W640649769 cites W2046056394 @default.
- W640649769 cites W2046115622 @default.
- W640649769 cites W2050668705 @default.
- W640649769 cites W2051654683 @default.
- W640649769 cites W2052002235 @default.
- W640649769 cites W2053399192 @default.
- W640649769 cites W2054410655 @default.
- W640649769 cites W2054969778 @default.
- W640649769 cites W2055227112 @default.
- W640649769 cites W2055727400 @default.
- W640649769 cites W2059788178 @default.
- W640649769 cites W2065013306 @default.
- W640649769 cites W2065531835 @default.
- W640649769 cites W2067621802 @default.
- W640649769 cites W2067786054 @default.
- W640649769 cites W2069716334 @default.
- W640649769 cites W2070892791 @default.
- W640649769 cites W2071003117 @default.
- W640649769 cites W2071417609 @default.
- W640649769 cites W2073452764 @default.
- W640649769 cites W2074218379 @default.
- W640649769 cites W2081766809 @default.
- W640649769 cites W2082517025 @default.
- W640649769 cites W2082646605 @default.
- W640649769 cites W2084299154 @default.
- W640649769 cites W2085408490 @default.
- W640649769 cites W2086839615 @default.
- W640649769 cites W2093090186 @default.
- W640649769 cites W2095991654 @default.
- W640649769 cites W2096729913 @default.
- W640649769 cites W2097122956 @default.
- W640649769 cites W2106389793 @default.
- W640649769 cites W2108784130 @default.
- W640649769 cites W2113403117 @default.
- W640649769 cites W2118182947 @default.
- W640649769 cites W2118334264 @default.
- W640649769 cites W2129870058 @default.
- W640649769 cites W2138786351 @default.
- W640649769 cites W2141028564 @default.
- W640649769 cites W2145619152 @default.
- W640649769 cites W2149307798 @default.
- W640649769 cites W2151529013 @default.
- W640649769 cites W2325493385 @default.
- W640649769 cites W2327801799 @default.
- W640649769 doi "https://doi.org/10.1016/j.dsr2.2015.06.016" @default.
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