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Horizontal Plate Motion: A Key Allocyclic Factor in the Evolution of the Great Barrier Reef | | P J Davies
; P A Symonds
; D A Feary
; C J Pigram
; | | Date: |
18 Dec 1987 | | Journal: | Science, 238 (4834), 1697-1700 | | Abstract: | The Great Barrier Reef complex of northeastern Australia thins dramatically and becomes younger from north to south. These variations are a consequence of the Cenozoic northward movement of the Indian-Australian plate. The temperate climatic conditions that applied off northeast Australia during the early Tertiary were progressively replaced by tropical conditions. The present-day south-to-north facies distribution along the eastern Australian continental margin mimics the Cenozoic vertical facies sequence through the northern part of the Great Barrier Reef region. | | Source: | PubMed, pmid17737670 doi: 10.1126/science.238.4834.1697 | | Services: | Forum | Review | Favorites | |
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