a (anorthic) = triclinic system, CM 25, [removed]A.1 = kaolinite or saggar-clay, Robertson[removed]AII = anhydrite, AM 91, [removed]aabam = lead, de Fourestier[removed]aanerödite = samarskite-(Y), AM 9, 62 (19

First Page		Document Content
Date: 2012-08-14 01:41:49 Amphibole group Asbestos Dielectrics Quartz Agate Riebeckite Jadeite Tremolite Aegirine Crystallography Silicate minerals Chemistry		a (anorthic) = triclinic system, CM 25, [removed]A.1 = kaolinite or saggar-clay, Robertson[removed]AII = anhydrite, AM 91, [removed]aabam = lead, de Fourestier[removed]aanerödite = samarskite-(Y), AM 9, 62 (19 Add to Reading List Source URL: www.minrec.org Download Document from Source Website File Size: 572,27 KB Share Document on Facebook

	GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L21305, doi:2005GL023522, 2005 High-pressure sound velocities and elasticity of aluminous MgSiO3 perovskite to 45 GPa: Implications for lateral heterogeneity in Earth’s l DocID: 1rrry - View Document
	Deep Sea Drilling Project Initial Reports Volume 93 DocID: 1rlku - View Document
	GEOPHYSICAL RESEARCH LETTERS, VOL. 37, L15304, doi:2010GL043689, 2010 Very low sound velocities in iron‐rich (Mg,Fe)O: Implications for the core‐mantle boundary region J. K. Wicks,1 J. M. Jackson,1,2 and W. DocID: 1rjq4 - View Document
	KIMBERLITES Kimberlite is an ultrabasic olivine-rich igneous rock called peridotite. Peridotites occur at great depths in the earth in a layer called the mantlemiles below the surface). At this depth the combi DocID: 1reER - View Document
	Deep Sea Drilling Project Initial Reports Volume 94 DocID: 1raPP - View Document