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LIU Xinying. Sequence and Depositional Characteristics in Synrift stage,  Sunda Basin, Indonesia[J]. Acta Sedimentologica Sinica, 2009, 27(2): 280-288.
Citation: LIU Xinying. Sequence and Depositional Characteristics in Synrift stage,  Sunda Basin, Indonesia[J]. Acta Sedimentologica Sinica, 2009, 27(2): 280-288.

Sequence and Depositional Characteristics in Synrift stage,  Sunda Basin, Indonesia

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  • Corresponding author: LIU Xinying
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2009-04-10
  • With the application of the theory of highresolution sequence stratigraphy referred to the core and seismic and logging data, the sequence framework was established within the synrifting of Sunda basin based on the well to seismic calibration. Six sequence boundaries are identified by which five sequences are divided. At the same time, the source direction and sedimentary facies of each sequence are analyzed. The basin developed depositional system of fan delta, braided channel delta, fluvial, delta, Nearshore Subaqueous Fans and beach, which changed greatly in different time and position. Compared to the typical rifted basin in East China, Sunda basin has short duration of synrifting and seldom developed subsidiary fracture accompanying with the main fracture. The duration of lacustrine basin was shorter and the water depth was shallower than the basin in East China.

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  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2009-04-10

Sequence and Depositional Characteristics in Synrift stage,  Sunda Basin, Indonesia

    Corresponding author: LIU Xinying

Abstract: With the application of the theory of highresolution sequence stratigraphy referred to the core and seismic and logging data, the sequence framework was established within the synrifting of Sunda basin based on the well to seismic calibration. Six sequence boundaries are identified by which five sequences are divided. At the same time, the source direction and sedimentary facies of each sequence are analyzed. The basin developed depositional system of fan delta, braided channel delta, fluvial, delta, Nearshore Subaqueous Fans and beach, which changed greatly in different time and position. Compared to the typical rifted basin in East China, Sunda basin has short duration of synrifting and seldom developed subsidiary fracture accompanying with the main fracture. The duration of lacustrine basin was shorter and the water depth was shallower than the basin in East China.

LIU Xinying. Sequence and Depositional Characteristics in Synrift stage,  Sunda Basin, Indonesia[J]. Acta Sedimentologica Sinica, 2009, 27(2): 280-288.
Citation: LIU Xinying. Sequence and Depositional Characteristics in Synrift stage,  Sunda Basin, Indonesia[J]. Acta Sedimentologica Sinica, 2009, 27(2): 280-288.

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