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Volume 28 Issue 4
Jul 2017
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Peng Zhang, Lianfu Mei, Ping Xiong, Xiaolin Hu, Renyuan Li, Huaning Qiu. Structural Features and Proto-Type Basin Reconstructions of the Bay of Bengal Basin: A Remnant Ocean Basin Model. Journal of Earth Science, 2017, 28(4): 666-682. doi: 10.1007/s12583-017-0750-8
Citation: Peng Zhang, Lianfu Mei, Ping Xiong, Xiaolin Hu, Renyuan Li, Huaning Qiu. Structural Features and Proto-Type Basin Reconstructions of the Bay of Bengal Basin: A Remnant Ocean Basin Model. Journal of Earth Science, 2017, 28(4): 666-682. doi: 10.1007/s12583-017-0750-8

Structural Features and Proto-Type Basin Reconstructions of the Bay of Bengal Basin: A Remnant Ocean Basin Model

doi: 10.1007/s12583-017-0750-8
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  • Remnant ocean basin is a key to understand the plate suturing and subsequent uplift and erosion of orogen. The Bay of Bengal Basin (BOBB) provides a typical example to analyze the remnant ocean basin structures, evolution, and relationships between depositional filling and uplifting of the Himalayan Orogen. Thirty-nine seismic profiles as well as interval velocities of well BODC3 were used to compile isopach maps of the basin. Among the seismic data, 26 seismic profiles were applied to establish 8 cross sections. The cross sections suggest the basin is asymmetric, bounded to the west by the eastern continental margin of India (ECMI) with graben-horst and to the east by the Sunda convergence margin dominated by trench-arc system. The BOBB is characterized by a prominent down flexure structures caused by huge amount of Bengal fan turbidite sediments accumulation. Our isopach maps and chronology data collected from adjacent regions reveal the initial development and fast southward growth of the Bengal fan were related to the early and major stage uplift and erosion of the Himalayan Orogen, respectively. The BOBB has experienced a critical transition from an ocean basin to a remnant ocean basin at Late Oligocene. Such basin structures and evolution features indicate the BOBB provides whole records of oblique convergence of the India and Asia plates, and the early and major stage evolution of the Himalayan Orogen.

     

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