【摘 要】
：
Controlled by the NE-and NW-trending faults the Hanjiang Delta formed in the Early Quaternary received deposits in the Middle Quaternary, continued to develop
【机 构】
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Guangdong Bureau of Seismology, Guangzhou
【出 处】
：
Acta Oceanologica Sinica
论文部分内容阅读
Controlled by the NE-and NW-trending faults the Hanjiang Delta formed in the Early Quaternary received deposits in the Middle Quaternary, continued to develop since the Holocene, and subsided at a velocity of 1 mm/yr. About 2000-3000 years BP the Hanjiang Delta began to uplift and became a land. Its formation and development are controlled by faulting. Early and late developments are controlled by the NE-and NW-trending fractures, respectively, indicating the rebirth and Intense activity of the latter.
Controlled by the NE-and NW-trending faults the Hanjiang Delta formed in the Early Quaternary received deposits in the Middle Quaternary, continued to develop since the Holocene, and subsided at a velocity of 1 mm / yr. About 2000-3000 years BP the Its formation and development are controlled by faulting. Early and late developments are controlled by the NE-and NW-trending fractures, respectively, indicating the rebirth and Intense activity of the latter.
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