塔斯曼半岛的勘察地质地貌

Q3 Multidisciplinary Papers and Proceedings - Royal Society of Tasmania Pub Date : 1986-11-01 DOI:10.26749/rstpp.120.1.7

MR Banks, EA Colhoun, R. Ford, E. Williams

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引用次数: 7

摘要

在塔斯马尼亚东南部的塔斯曼半岛上，几乎水平的二叠纪海相和三叠纪非海相岩石被侏罗纪白云岩侵入，第三纪玄武岩被侏罗纪和更古老的岩石断裂和覆盖，形成了一个悬崖状的海岸线，具有许多以其壮观和罕见而闻名的侵蚀特征。这些特征形成了一种自我更新的经济资产。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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A reconnaissance geology and geomorphology of Tasman Peninsula

On Tasman Peninsula, south-eastern Tasmania, almost horizontal Permian marine and Triassic non-marine rocks were intruded by Jurassic dolerite, faulted and overlain by Tertiary basalt Marine processes operating on the Jurassic and older rocks have produced a cliffed coastline with many erosional features widely noted for their grandeur and rarity. These features form a self-renewing economic asset.

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来源期刊

Papers and Proceedings - Royal Society of Tasmania Multidisciplinary-Multidisciplinary

CiteScore

0.60

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0.00%

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