Thinned crustal structure and tectonic boundary of the Nansha Block, southern South China Sea

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• 作者：Miao Dong ; Shi-Guo Wu ; Jian Zhang
• 关键词：Moho ; Curie point depth ; Crustal structure ; Tectonic boundary ; Nansha Block ; South China Sea
• 刊名：Marine Geophysical Research
• 出版年：2016
• 出版时间：December 2016
• 年：2016
• 卷：37
• 期：4
• 页码：281-296
• 全文大小：
• 刊物类别：Earth and Environmental Science
• 刊物主题：Oceanography; Geophysics/Geodesy; Earth Sciences, general; Offshore Engineering;
• 出版者：Springer Netherlands
• ISSN：1573-0581
• 卷排序：37

文摘

The southern South China Sea margin consists of the thinned crustal Nansha Block and a compressional collision zone. The Nansha Block’s deep structure and tectonic evolution contains critical information about the South China Sea’s rifting. Multiple geophysical data sets, including regional magnetic, gravity and reflection seismic data, reveal the deep structure and rifting processes. Curie point depth (CPD), estimated from magnetic anomalies using a windowed wavenumber-domain algorithm, enables us to image thermal structures. To derive a 3D Moho topography and crustal thickness model, we apply Oldenburg algorithm to the gravity anomaly, which was extracted from the observed free air gravity anomaly data after removing the gravity effect of density variations of sediments, and temperature and pressure variations of the lithospheric mantle. We found that the Moho depth (20 km) is shallower than the CPD (24 km) in the Northwest Borneo Trough, possibly caused by thinned crust, low heat flow and a low vertical geothermal gradient. The Nansha Block’s northern boundary is a narrow continent–ocean transition zone constrained by magnetic anomalies, reflection seismic data, gravity anomalies and an interpretation of Moho depth (about 13 km). The block extends southward beneath a gravity-driven deformed sediment wedge caused by uplift on land after a collision, with a contribution from deep crustal flow. Its southwestern boundary is close to the Lupar Line defined by a significant negative reduction to the pole (RTP) of magnetic anomaly and short-length-scale variation in crustal thickness, increasing from 18 to 26 km.