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    Volume 35 Issue 4
    Jul.  2010
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    ZHAO Li-hong, JIN Xiang-long, GAO Jin-yao, LI Jia-biao, CHU Feng-you, 2010. The Effective Elastic Thickness of Lithosphere in the Mid-West Pacific and Its Geological Significance. Earth Science, 35(4): 637-644. doi: 10.3799/dqkx.2010.078
    Citation: ZHAO Li-hong, JIN Xiang-long, GAO Jin-yao, LI Jia-biao, CHU Feng-you, 2010. The Effective Elastic Thickness of Lithosphere in the Mid-West Pacific and Its Geological Significance. Earth Science, 35(4): 637-644. doi: 10.3799/dqkx.2010.078

    The Effective Elastic Thickness of Lithosphere in the Mid-West Pacific and Its Geological Significance

    doi: 10.3799/dqkx.2010.078
    • Received Date: 2009-10-20
    • Publish Date: 2010-07-01
    • The Mid-West Pacific region is featured with the oldest oceanic crust, the most complicated magnetic anomaly lineation, the densest seamounts, the most peculiar geological feature and the strongest tectonic activity. To research tectonic genesis of these intraplate seamounts, this paper calculates the effective elastic thickness of the lithosphere (Te) with the elastic plate flexure based on the plate tectonic theory in the Mid-West Pacific. As a whole, Te slowly drops from the northwest part to the southeast part in the region. Te of the MST is higher in the middle of the trail than that in the north and the south parts. Te of the MPM is higher in the west part of the mountains than that in the east part. Furthermore, Te of these two typical areas is close to that of the present French Polynesia region. Thus, these seamounts were formed by the large volcanism which was produced by several hotspots during Cretaceous in the present French Polynesia region. And then these seamounts underwent some tectonic activities.

       

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