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Date: 2009-01-14 01:27:23 Historical geology Economic geology Planetary geology Geochronology Regolith Saprolite Paleomagnetism Yilgarn Craton Appearance Event Ordination Geology Planetary science Sedimentology		Microsoft Word - 034_Anand_R_Final.doc Add to Reading List Source URL: www.crcleme.org.au Download Document from Source Website File Size: 926,30 KB Share Document on Facebook

	EARTH SURFACE PROCESSES AND LANDFORMS Earth Surf. Process. LandformsCopyright © 2013 John Wiley & Sons, Ltd. Published online in Wiley Online Library (wileyonlinelibrary.com) DOI: esp.3502 DocID: 1rqqn - View Document
	Sharp decrease in long-term chemical weathering rates along an altitudinal transect Clifford S. Riebe* Department of Earth and Planetary Science, University of California, Berkeley, CA, eley.e DocID: 1rp9a - View Document
	Geochimica et Cosmochimica Acta, Vol. 67, No. 22, pp. 4411– 4427, 2003 Copyright © 2003 Elsevier Ltd Printed in the USA. All rights reserved $30.00 ⫹ .00 Pergamon DocID: 1qW6w - View Document
	Strong tectonic and weak climatic control of long-term chemical weathering rates Clifford S. Riebe* James W. Kirchner Department of Earth and Planetary Science, University of California, Berkeley, California, DocID: 1qPVm - View Document
	Yilgarn Craton: A case study in regolith formation The Yilgarn Craton is one of the largest segments of Archaen crust on Earth. It has an area of about 657,000 km2 (26% of WA) and is situated in the Precambrian Western S DocID: 1qPhN - View Document