L. H. Ahrens, J. B. Dawson and A. R. Duncan (Eds.)'s Physics and Chemistry of the Earth. The Contents of This PDF

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By L. H. Ahrens, J. B. Dawson and A. R. Duncan (Eds.)

ISBN-10: 0080180175

ISBN-13: 9780080180175

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Read Online or Download Physics and Chemistry of the Earth. The Contents of This Volume Include Most of the Papers Presented at the First International Conference on Kimberlites Held in Cape Town from 24th to 28th September 1973 PDF

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Additional resources for Physics and Chemistry of the Earth. The Contents of This Volume Include Most of the Papers Presented at the First International Conference on Kimberlites Held in Cape Town from 24th to 28th September 1973

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EMELEUS The host rock around most sheets is invariably jointed parallel to the intrusion margins in the manner of the Nigerdlikasik dyke; jointing has developed at various intensities in both the granite and gneiss. A tendency for the sheets to erode into the granite giving rise to small caves and rock shelters has resulted in large collapse structures, especially where the jointing is very closely spaced, with corresponding concealment of kimberlite betrayed only by loose blocks in scree. Selective ice action has plucked away large amounts of material producing bench features sometimes 20-30 m wide and corresponding cliflF features or overhangs.

283-6. SHOEMAKER, E. , ROACH, C. H. and BYERS, F. , Jr. (1962) Diatremes and uranium deposits in the Hopi Buttes, Arizona. Geol. Soc. Amer. Bull. ), pp. 327-55. THORARINSSON, S. (1967) Some problems of volcanism in Iceland. Geol. Rundschau 57, 1-20. WALKER, G. P. L. and CROASDALE, R. (1972) Characteristics of some basaltic pyroclastics. Bull. Volcano logique 35, 303-17. WHYTE, F. (1968) Lower Carboniferous volcanic vents in the West of Scotland. Bull. Volcano logique 32, 253-68. WOOLSEY, T. , MCCALLUM, M.

The planar foliation in the gneisses and well-developed bedding surfaces in the supracrustal rocks have little or no' influence on the attitude of the sheets which in the supracrustal succession cut across bedding at very acute angles. The massive basement gneisses and supracrustal rocks where they are tightly folded and indurated develop the characteristic well jointed or shattered aspect familar in the Pyramidefjeld complex. One unique feature on Midternaes is the association of calcite metasomatism with sill emplacement in the supracrustal succession.

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Physics and Chemistry of the Earth. The Contents of This Volume Include Most of the Papers Presented at the First International Conference on Kimberlites Held in Cape Town from 24th to 28th September 1973 by L. H. Ahrens, J. B. Dawson and A. R. Duncan (Eds.)


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