The Problem of the Association of Acid and Basic Rocks in Central Complexes
One of the outstanding problems of petrogenesis at the present time is that offered by the remarkable association of sharply contrasted acid and basic rocks (e.g. granite-gabbro; granophyredolerite; pitchstone-tholeiite; and rhyolite-basalt) in igneous complexes such as those of the British Tertiary...
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Language: | English |
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Cambridge University Press (CUP)
1931
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Online Access: | http://dx.doi.org/10.1017/s0016756800087197 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800087197 |
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crcambridgeupr:10.1017/s0016756800087197 2024-03-03T08:45:43+00:00 The Problem of the Association of Acid and Basic Rocks in Central Complexes Holmes, Arthur 1931 http://dx.doi.org/10.1017/s0016756800087197 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800087197 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 68, issue 6, page 241-255 ISSN 0016-7568 1469-5081 Geology journal-article 1931 crcambridgeupr https://doi.org/10.1017/s0016756800087197 2024-02-08T08:37:29Z One of the outstanding problems of petrogenesis at the present time is that offered by the remarkable association of sharply contrasted acid and basic rocks (e.g. granite-gabbro; granophyredolerite; pitchstone-tholeiite; and rhyolite-basalt) in igneous complexes such as those of the British Tertiary Province and those of the great lopoliths of Duluth and Sudbury in North America and the Bushveld in South Africa. The contrast was first recognized in the lavas of Iceland by Bunsen (1) and it led him to the conception that two fundamental magmas, respectively acid and basic, were concerned in the genesis of the igneous rocks of Iceland and similar provinces elsewhere. Bunsen's view, however, has had little influence in the development of petrological philosophy. The petrologists of the Geological Survey in this country, and Bowen and others in North America, have assembled a very weighty and reasonable mass of field and laboratory evidence supporting the hypothesis that the acid rocks are residual products arising from the crystallization-differentiation of basaltic magmas. In the recently published Ardnamurchan Memoir (2), for example, it is claimed that as a result of the early extraction from the Plateau Magma of olivine, pyroxenes, basic plagioclase, and iron ores, the residual magma would reach a composition “which would find expression as quartz-doleritic rocks with an acid mesostasis capable of mechanical separation and a separate existence as acid lavas or intrusions” (p. 95). Bunsen's two magmas are thus regarded as successive products from a single parent stock. Article in Journal/Newspaper Iceland Cambridge University Press Geological Magazine 68 6 241 255 |
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Cambridge University Press |
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English |
topic |
Geology |
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Geology Holmes, Arthur The Problem of the Association of Acid and Basic Rocks in Central Complexes |
topic_facet |
Geology |
description |
One of the outstanding problems of petrogenesis at the present time is that offered by the remarkable association of sharply contrasted acid and basic rocks (e.g. granite-gabbro; granophyredolerite; pitchstone-tholeiite; and rhyolite-basalt) in igneous complexes such as those of the British Tertiary Province and those of the great lopoliths of Duluth and Sudbury in North America and the Bushveld in South Africa. The contrast was first recognized in the lavas of Iceland by Bunsen (1) and it led him to the conception that two fundamental magmas, respectively acid and basic, were concerned in the genesis of the igneous rocks of Iceland and similar provinces elsewhere. Bunsen's view, however, has had little influence in the development of petrological philosophy. The petrologists of the Geological Survey in this country, and Bowen and others in North America, have assembled a very weighty and reasonable mass of field and laboratory evidence supporting the hypothesis that the acid rocks are residual products arising from the crystallization-differentiation of basaltic magmas. In the recently published Ardnamurchan Memoir (2), for example, it is claimed that as a result of the early extraction from the Plateau Magma of olivine, pyroxenes, basic plagioclase, and iron ores, the residual magma would reach a composition “which would find expression as quartz-doleritic rocks with an acid mesostasis capable of mechanical separation and a separate existence as acid lavas or intrusions” (p. 95). Bunsen's two magmas are thus regarded as successive products from a single parent stock. |
format |
Article in Journal/Newspaper |
author |
Holmes, Arthur |
author_facet |
Holmes, Arthur |
author_sort |
Holmes, Arthur |
title |
The Problem of the Association of Acid and Basic Rocks in Central Complexes |
title_short |
The Problem of the Association of Acid and Basic Rocks in Central Complexes |
title_full |
The Problem of the Association of Acid and Basic Rocks in Central Complexes |
title_fullStr |
The Problem of the Association of Acid and Basic Rocks in Central Complexes |
title_full_unstemmed |
The Problem of the Association of Acid and Basic Rocks in Central Complexes |
title_sort |
problem of the association of acid and basic rocks in central complexes |
publisher |
Cambridge University Press (CUP) |
publishDate |
1931 |
url |
http://dx.doi.org/10.1017/s0016756800087197 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800087197 |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Geological Magazine volume 68, issue 6, page 241-255 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800087197 |
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Geological Magazine |
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68 |
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6 |
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241 |
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255 |
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1792501363880493056 |