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2020 Vol. 40, No. 4
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DONG Hao, DAI Liming, LI Sanzhong, HU Zeming. Dynamic connection between Archean magma vents and Dome-and-Keel Structures[J]. Marine Geology & Quaternary Geology, 2020, 40(4): 116-126. doi: 10.16562/j.cnki.0256-1492.2020050301
Citation: DONG Hao, DAI Liming, LI Sanzhong, HU Zeming. Dynamic connection between Archean magma vents and Dome-and-Keel Structures[J]. Marine Geology & Quaternary Geology, 2020, 40(4): 116-126. doi: 10.16562/j.cnki.0256-1492.2020050301
shu

Dynamic connection between Archean magma vents and Dome-and-Keel Structures

  • 1.

    Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Institute for Advanced Ocean Study, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China

  • 2.

    Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China

More Information
Received Date:  03 May 2020
Revised Date:  19 May 2020
Publish Date:  25 August 2020
    Abstract

  • Magmatism is the main method for lithospheric cooling in Archean. It not only produces new materials, but also provides power for lithospheric deformation. The records of Archean deformation remained up to present suggest that the dome-and keel-structure related to the vertical movement are widely developed in the interiors of continental cratons at that time. However, it is not clear how the vertical structures work with the Archean magmatic activity. In order to make the study more intuitively, we made a two-dimensional numerical model in size of 879 × 400 km2 based on the finite difference numerical simulation method and then tried to work out the intrusion process by setting magma conditions. The experimental results show that the magma vent array weakens the lithosphere and causes strong deformation of the lithosphere. The TTG domes are formed on the top of the magma vents. There is a negative topography between the magma channels. There is a negative topography, a depression, between the dense magma vents. During the evolution of the dome, it will expand horizontally resulting in the narrowing of the greenstone belt and the appearance of " bag" style. They constitute the dome-and keel-structure. In our study, considering magmatism as a condition of lithosphere deformation is consistent with the facts from the Archean geological background. The magma vent array, as an important factor for lithosphere deformation, provides driving force for the formation of the dome-and-keel structure.

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