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Distribution of alkaline intrusive rocks and related metallic ore deposits of China
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The petrology of miarolitic granite along the southeast coast of Fujian province and their generation
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Tectonic environments of alkaline granites and their discriminating indications
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Age and genesis of the alkaline rocks in Northern Hubei province
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Age and distribution of alkaline and subalkaline intrusive rocks in Northern China
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Abstract: On the basis of the geological data from 220 intrusions and isotope ages of 115 rock bodies, the paper discusses the distribution of 18 alkaline intrusive rock belts along deep faults and their relations to the plate tectonic activity. In view of the presence of a large amount of Variscan alkaline rocks of deep‐source character, it is inferred that mantle diapirism was very strong in China during the Variscan. Besides anorogenic and postorogenic alkaline granites, there also occur alkaline granites formed in the terminal orogenic stage when the regional tectonic activity was of compressional nature. Finally, the paper discusses the tectonic environment of the Maoniuping nordmarkite in Mianning county, Sichuan province, and the authors consider it to be a compressional environment originating after rift closing.
Acta Geologica Sinica (English Edition) – Wiley
Published: Dec 1, 1998
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