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ZHANG HUNAN. 1985. ON THE RELATIONSHIP BETWEEN FAULTNG AND FORMATION AS WELL AS DEVELOPMENT OF HANJIANG DELTA. Acta Oceanologica Sinica, (2):266-275
ON THE RELATIONSHIP BETWEEN FAULTNG AND FORMATION AS WELL AS DEVELOPMENT OF HANJIANG DELTA
ON THE RELATIONSHIP BETWEEN FAULTNG AND FORMATION AS WELL AS DEVELOPMENT OF HANJIANG DELTA
Received:January 17, 1984  Revised:July 10, 1984
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ZHANG HUNAN Guangdong Bureau of Seismology, Guangzhou 
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Abstract:
      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.
中文摘要:
      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 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.
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