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南沙群岛区域地质地貌与古海洋 被引量:6

REGIONAL GEOLOGY, GEOMORPHOLOGY AND PALEOOCEANOGRAPHY OF THE NANSHA ISLANDS
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摘要 本文论述了南沙群岛海底地形、海底沉积物、区域地质、珊瑚礁地质地貌和区域古海洋。 ome characteristics hi the Nansha Islands , such as bottom relief, bottom sediments,regional geology, geology and geomorphology of coral reefs, and regional paleooceanography are discussed in this paper. The tectonics of the Nansha Islands can be divided into Central Basin Fault-Spread Region, Nansha Faulted Platform Region, and Zengmu Graben Zone.And correspondingly the bottom reliefs are the abyssal plain, Nansha sea plateau, upper continental slope, and continental shelf. Since Cenozoic era, the seas of the Nansha Islands have always been tropical seas. The bioherms have been developing since Late OligoceneEpoch, and the lime-sand islands were formed after Middle Holocene in the seas.Paleoclinlate changed synchronously with the whole world over the past 900 000 years , but the temperatures between glacisl epoch and interglacial stage varied little. Oscillatory paleosea-level change, Caused by the paleoclimate change, resulted in the alternation between emergence and submergence of continent shelf and islands, and in the change of surfacewater circulation model.
出处 《热带地理》 北大核心 1995年第2期128-137,共10页 Tropical Geography
关键词 南沙群岛 地质 地貌 古海洋 区域地貌 Nansha Islands Geology Geomorphology Paleooceanography
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  • 1李毓英.南沙群岛太平岛地质概况[J]地质论评,1948(Z3).
  • 2曾昭璇.南海环礁的若干地貌特征[J]海洋通报,1984(03).
  • 3曾昭璇.中国环礁的类型划分[J]海洋通报,1982(04).
  • 4李毓英.南沙群岛太平岛地质概况[J]地质论评,1948(Z3).

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