by Unknown | at Tuesday, January 27, 2015
by Unknown | at Tuesday, April 29, 2014

Copyright © 1987 K. R. McClayReprinted in September 1991 byJohn Wiley & Sons Ltd, The Atrium, Southern Gate,Chichester, West Sussex PO19 8SQ, EnglandFirst published in 1987 by Open University PressReprinted 1991, 1992, 1994, 1995, 1996, 1997 (twice), 1999, 2000,2001, 2002, 2003 (three times), 2005, 2006, 2007All rights reservedNo part of this book may be reproduced by any means,or transmitted, or translated into a...
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by Unknown | at Tuesday, April 29, 2014

The following exercises guide you in progressive steps through theanalysis and interpretation of geological maps. This is an introductory course that will give you basic, fundamental skills. The course will build upon the work you did in the first few lab classes in GEOL 112 and you should review those lab classes. Some of these exercises will be completed on the Wherewithal Fieldclass....
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by Unknown | at Tuesday, April 29, 2014

GEOL302 INDEPENDENT FIELD STUDIES 18 hcpsPREREQUISITES: GEOL 251 and 252CO-REQUISITES: GEOL 344TEACHING STAFF: AllFORMAT: Full year; no lectures, no laboratories.FIELDWORK:Independent field-based project.ASSESSMENT:• 15% Field data: Due 24th May: 4pm.• 10% Talk: 12th July (provisional)• 75% Project report (65%) and final graphic syntheses (e.g. final map, cross sections, etc.. 10%).Due 16th August: 4pm.• Acceptance of project is dependent upon all samples, thin sections...
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by Unknown | at Tuesday, April 29, 2014

ABSTRACT In this paper we have focused on fundamental processes that are important for understanding the electrical properties of materials, both single crystal minerals and igneous rocks, both laboratory-grown and from natural environments. The prevailing view in the geophysics community is that the electrical conductivity structure of the Earth’s continental crust over the 5-35 km depth range can best be understood by...
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by Unknown | at Tuesday, April 29, 2014

Abstract- The performance of various shaly sand saturation equations was compared to the water saturation calculated from drainage capillary pressure. T he wireline logging, mud logging, well testing, and core data had been carefully evaluated during the processing of the data; therefore, data quality was thought to be good. Almost all kinds of petrophysical parameters were used for log interpretation in the area...
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