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福建构造地貌发育机制初探

A Preliminary Study of Formation Mechanism of Tectonic Landform of Fujian

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【作者】 李祖光

【Author】 LI Zu-guang (Department of Geography)

【机构】 福建师范大学地理系

【摘要】 中、新生代以来太平洋板块和菲律宾板块向欧亚大陆板块俯冲,产生的水平应力场,是福建构造活动的主要动力来源。在该应力场的作用下,形成了以北北东——北东向和北西向为主的断裂构造。本文着重论述在断裂构造控制下,福建构造地貌的形成机制,并探讨其空间的分布——纵列成条、横分为块、条块分明、以条为主的地貌景观。

【Abstract】 Ever since the Mesozoic and the Neozoic the horizontal stress field caused by the downward impact of the Philippine plate and the Pacific plate towards the Eurasia plate has been the principal dynamic source to bring about the tectonic activities in Fujian, and has formed the fracture structures that chiefly run NNE —NE and NW. This thesis puts its emphasis on the discussion of the formation mechanism of Fujian controlled by fracture structures. The thesis also studies the space distribution of the landforms-in distinctive shapes of strips running from north to south, of lumps from east to west with the former as the main structures.

  • 【文献出处】 福建师范大学学报(自然科学版) ,Journal of Fujian Normal University(Natural Science Edition) , 编辑部邮箱 ,1988年02期
  • 【被引频次】3
  • 【下载频次】126
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