Volume 25 Issue 5
Oct.  2019
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Article Contents
LI Sanzhong, CAO Xianzhi, WANG Guangzeng, et al., 2019. MESO-CENOZOIC TECTONIC EVOLUTION AND PLATE RECONSTRUCTION OF THE PACIFIC PLATE. Journal of Geomechanics, 25 (5): 642-677. DOI: 10.12090/j.issn.1006-6616.2019.25.05.060
Citation: LI Sanzhong, CAO Xianzhi, WANG Guangzeng, et al., 2019. MESO-CENOZOIC TECTONIC EVOLUTION AND PLATE RECONSTRUCTION OF THE PACIFIC PLATE. Journal of Geomechanics, 25 (5): 642-677. DOI: 10.12090/j.issn.1006-6616.2019.25.05.060


doi: 10.12090/j.issn.1006-6616.2019.25.05.060
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  • Received: 2019-08-10
  • Revised: 2019-09-28
  • Published: 2019-10-31
  • The Pacific Plate is the largest oceanic plate on the Earth since Mesozoic, but its original mechanism, structure and tectonic evolution are still unclear. The complexity of the interior of the Pacific Plate has not been taken seriously. Large igneous provinces, seamount chains, oceanic micro-blocks, continental micro-blocks and mantle micro-blocks in the deeper mantle in or under the Pacific Plate are well developed. The geodynamic implications of these complex intraplate or sub-plate structures need to be solved urgently. Based on the latest results of plate reconstruction, this paper attempts to analyze its kinematic process and to reveal the formation and evolution mechanism of the Pacific Plate. The results show that the Pacific Plate originated from the RRR triple junction, but it was not a pure oceanic plate. Its accretion and evolutionary processes have undergone a non-Wilson cycle model. Its margins have undergone the incorporation of some exotic continental or oceanic micro-blocks, and some new oceanic micro-blocks have involved and appeared in its interior for various reasons. It made the Pacific Plate show as a fragmented mosaic pattern. The Pacific Plate recorded important tectonic events interacting with the adjacent tectonic plates. At about 55 Ma, it began to subduct under the East Asian continental margin, resulting in a short NW-SE-directed extension of the East Asian continental margin, which was subsequently jointly controlled by the Indian-Eurasian collisional dynamic system and the Pacific subduction dynamic system, and generally formed some pull-apart basins under the right-lateral dextral strike slipping. Then due to subduction retreat, this region gradually developed a double subduction system. The Pacific Plate also recorded the deep-shallow coupling process, and the Pacific LLSVP in the lower mantle played a decisive role in the distribution of the upper lithospheric micro-plates and large igneous provinces. In addition, volcanic chains or hotspots not only reveal plate movement, but also reflect the process of material exchange between deep and shallow parts, and seamounts also reveal the mantle flow under the Pacific Plate. The mantle circulation is not a single convective cell, and the diversity of its convective pattern needs to be further studied.


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