Volume 42 Issue 11
Nov.  2017
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Article Navigation >  Earth Science  > 2017  >  42(11): 1883-1896
Liu Qianghu, Zhu Xiaomi, Li Shunli, Xu Changui, Du Xiaofeng, Li Huiyong, Shi Wenlong, 2017. Source-to-Sink System of the Steep Slope Fault in the Western Shaleitian Uplift. Earth Science, 42(11): 1883-1896. doi: 10.3799/dqkx.2017.119
Citation: Liu Qianghu, Zhu Xiaomi, Li Shunli, Xu Changui, Du Xiaofeng, Li Huiyong, Shi Wenlong, 2017. Source-to-Sink System of the Steep Slope Fault in the Western Shaleitian Uplift. Earth Science, 42(11): 1883-1896. doi: 10.3799/dqkx.2017.119
shu

Source-to-Sink System of the Steep Slope Fault in the Western Shaleitian Uplift

doi: 10.3799/dqkx.2017.119
  • 1.

    Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan 430074, China

  • 2.

    College of Geosciences, China University of Petroleum, Beijing 102249, China

  • 3.

    Tianjin Branch, China National Offshore Oil Corporation Limited, Tianjin 300459, China

  • Received Date: 2017-05-15
  • Publish Date: 2017-11-15
    Abstract
  • During the early stage of Palaeogene, western Shaleitian uplift and surrounding areas constituted a complete Source-to-Sink system under the control of steep slope fault. We analyzed the characteristics of Source-to-Sink elements (provenance system, sediment-routing system, and sedimentary system), discussed the relativities among the three elements and established the coupling model of steep slope fault based on detritus, thin section and the geophysical response datain this study. Results show that the provenance of western Shaleitian uplifts was filled by Proterozoic metamorphic rocks. Based on the Paleogene palaeo-geomorphology, we divided the provenance into four third-order catchment units, obtained the quantitative parameters of height difference and catchment area, and confirmed the distribution and scales of incised valleys and faulted-troughsediment-transport pathways. The facies architecture and sediment-dispersal characters of fan-deltas system in the third member of Eocene Shahejie Formation have been analyzed by the stratal slice images. Quantitative analysis of the parameters in the source-to-sink system show that the total sediment volume yielded by the eroded and weathered hinterland into the basin is closely related to the catchment area and the height difference of the hinterland. Then, the coupling model of source (migmatitic granite)-channel (incised valleys or fault-trough sediment-transport pathways)-sink (near-source coarse grain size fan delta-gravity flow-lake system) controlled by fault steep slopehas been established.

     

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