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Updated: Jul 11, 2026

Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar
07:14

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在纳兹卡板下面的沟平行流是由于地震异构性而产生的

R M Russo, P G Silver

    Science (New York, N.Y.)
    |February 25, 1994
    PubMed
    概括

    剪波分裂揭示了纳斯卡板下面的地幔流是水平的和与沟平行的,而不是二维的. 这种流动模式影响了南美和加勒比地区的板块构造和地质特征.

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