The characteristics and distribution of the Moho reflections in the South China Sea Oceanic Basin
- 1 February 2024
- journal article
- research article
- Published by Society of Exploration Geophysicists in Interpretation
- Vol. 12 (2) , SA17-SA27
Abstract
The distribution and characteristics of the Moho reflections (M-reflections) in oceanic basins record the seafloor spreading process and provide crucial insights into the formation and evolution of the oceanic basins. Approximately 20,000 km of multichannel seismic reflection sections are used to characterize the M-reflections and the crustal structures in the South China Sea oceanic subbasins. The identified M-reflections are mainly distributed in the northwest subbasin, the east subbasin, and the northern and southern flanks of the southwest subbasin (SWSB). They exhibit a banded distribution pattern in two-way traveltime along the north–south direction, with shallower depths observed in the central region and gradually deepening toward the northern and southern sides. In addition, the M-reflection amplitudes generally weaken, and the reflection events become less continuous as the igneous oceanic crust thins along with the seafloor spreading prior to the second ridge jump event. Ultimately, the M-reflection becomes indistinguishable in proximity to fossil spreading centers. These observations suggest a decreasing magma supply toward the cessation of the spreading. Despite the significance of Moho interface imaging at the crust-mantle boundary, the distinct M-reflections are absent in the SWSB and the vicinity of the Zhenbei-Huangyan Seamounts Chain, which are attributed to several factors, especially the vague nature of Moho interfaces.Keywords
Funding Information
- the project of China Geological Survey (DD20201118, DD20230069)
- PI Project of Southern Marine Science and Engineering Guangdong Laboratory (GML2020GD0802)
- the Major Program of Guangdong Basic and Applied Basic Research Foundation (2019B030302004)
- the Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (GML2019ZD0207)
- the Key Research and Development Project of Guangdong (2020B1111510001)
- the State Key Laboratory of Marine Geology, Tongji University (MGK1920)
- the project of China Geological Survey (DD20201118, DD20230069)
- PI Project of Southern Marine Science and Engineering Guangdong Laboratory (GML2020GD0802)
- the Major Program of Guangdong Basic and Applied Basic Research Foundation (2019B030302004)
- the Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (GML2019ZD0207)
- the Key Research and Development Project of Guangdong (2020B1111510001)
- the State Key Laboratory of Marine Geology, Tongji University (MGK1920)
This publication has 53 references indexed in Scilit:
- Sub-axial deformation in oceanic lower crust: Insights from seismic reflection profiles in the Enderby Basin and comparison with the Oman ophioliteEarth and Planetary Science Letters, 2021
- Lateral evolution of the rift-to-drift transition in the South China Sea: Evidence from multi-channel seismic data and IODP Expeditions 367&368 drilling resultsEarth and Planetary Science Letters, 2020
- Structures within the oceanic crust of the central South China Sea basin and their implications for oceanic accretionary processesEarth and Planetary Science Letters, 2018
- Postseafloor Spreading Volcanism in the Central East South China Sea and Its Formation Through an Extremely Thin Oceanic CrustGeochemistry, Geophysics, Geosystems, 2018
- Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Expedition 349Geochemistry, Geophysics, Geosystems, 2014
- Crustal thickness and Moho character of the fast‐spreading East Pacific Rise from 9°42′N to 9°57′N from poststack‐migrated 3‐D MCS dataGeochemistry, Geophysics, Geosystems, 2014
- Tracing the life history of a marginal sea—On “The South China Sea Deep” Research ProgramChinese Science Bulletin, 2012
- Crustal features of the northeastern South China Sea: insights from seismic and magnetic interpretationsMarine Geophysical Research, 2012
- Geomagnetic Polarity Time Scale2012
- Mantle reflections beneath the crestal zone of the East Pacific Rise from multi-channel seismic dataMarine Geology, 1980