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Sericite from
Juan Tabo area, Placitas Mining District, Bernalillo County, New Mexico, USA


Locality type:Area
Classification
Species:Muscovite var: Sericite
Formula:KAl2(AlSi3O10)(OH)2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Sericite data
Locality Data:Click here to view Juan Tabo area, Placitas Mining District, Bernalillo County, New Mexico, USA
Data Identifiers
Mindat Occurrence Record ID:238889
Long-form Identifier:1:3:238889:2
GUID (UUID V4):2dd59de6-2be1-4d4d-8d41-c1b8b0d3b46e
Nearest other occurrences of Sericite
30.6km (19.0 miles) Carache Canyon breccia, Old Placers District, Santa Fe County, New Mexico, USA
33.1km (20.6 miles) Ortiz Open Pit Mine, Ortiz Project, Golden, Old Placers District, Santa Fe County, New Mexico, USA
34.5km (21.4 miles) Cunningham mine, Old Placers District, Santa Fe County, New Mexico, USA
34.5km (21.5 miles) Ortiz Project, Golden, Old Placers District, Santa Fe County, New Mexico, USA
42.6km (26.5 miles) Grand Central Mine, Cerrillos District, Santa Fe County, New Mexico, USA
42.8km (26.6 miles) Cash Entry mine, Cerrillos District, Santa Fe County, New Mexico, USA
44.0km (27.4 miles) Cerro Colorado, Bernalillo County, New Mexico, USA
62.0km (38.5 miles) El Cuervo Butte, El Cuervo Butte Mining District, Santa Fe County, New Mexico, USA
94.2km (58.5 miles) Pecos Mine (Hamilton Mine; Cowles Mine), Willow Creek District, San Miguel County, New Mexico, USA
97.0km (60.3 miles) Morningstar Prospect, Jemez pumice Mining District, Sandoval County, New Mexico, USA
References
Reference Search (possible matching items)
Book (edition)
org/details/mineralsofnewmexOOnort MINERALS OF NEW MEXICO Before all things, there which has them ...that 1825 mining opened the West- . —Charles W. Henderson, 1933 MINERALS of New Mexico STUART A...Mew Mexico PROPERTY OF HBSIER JR. HIGH SCH LIBRARY Revised Edition UNIVERSITY OF NEW MEXICO PRESS...ALBUQUERQUE © 1944. 1959. UNIVERSITY OFNEW MEXICO PRESS ALL RIGHTS RESERVED REVISED EDITION LIBRARY...BOUND AT THE UNIVERSITY OF NEW MEXICO PRINTING PLANT ALBUQUERQUE, NEW MEXICO, U. S. A. FOR IVAH 1
Report (issue)
Department of Geology University of New Mexico Albuquerque, New Mexico 87131 Barbara J. Tewksbury Department...Department of Geology Hamilton College Clinton, New York 13323 ~ ‘PAPER 235 1989 © 1989 The Geological...CIP Cover Photo: Proterozoic rocks of northern New Mexico are separated into two tectonometamorphic plates...metamorphism of Proterozoic rocks in northern New Mexico ............ Jeffrey A. Grambling, Michael L...and plutons of the Cimarron Canyon area, north-central New Mexico Reinhard A. Wobus Geology and geochemistry
Journal (article/letter/editorial)
sillimanite lamella and the andalusite host. (c) Selected-area electron diffraction (SAED) pattern at the interface...breaking and, after slight displacement of the cations, new formation of Si-O and Al-O bonds. Diffusion distances...andalusite and sillimanite may co-exist over an area corresponding to a large temperature interval and...reactions between andalusite, “sericite” and sillimanite, Mount Franks area, Willyama Complex, N.S.W. Tectonophysics...Mineral Sciences, 457 p. Cambridge University Press, New York. Rosenfeld, J.L. (1969) Stress effects around
Journal (article/letter/editorial)
au) 2 Department of Applied Geology, University of New South Wales, NSW 2052, Australia ABSTRACT The Albany–Fraser...Australo-Antarctic cratonic assembly during the Mesoproterozoic. New petrologic and thermobarometric data from the Coramup...metamorphism and D2 deformation. In a companion paper, new structural and U–Pb SHRIMP zircon data are presented...Coramup Gneiss (i.e. the Butty Head– Butty Harbour area; Fig. 3b,c), and comprise NE-trending, subvertical...shear zone Trend of dominant gneissosity Inland area (no outcrop) Beach (sand and boulders) Granitic
Journal (article/letter/editorial)
spectacularly preserved (Fig. 2c). Up to 80% of the area of the symplectite is occupied by spinel that occurs...diaspore and cordierite to pinite or fine-grained sericite, but the symplectite textures are still well preserved...points at higher pressures become metastable and new ones appear. On the other hand, our grid is in agreement...calculated for a local composition corresponding to the area surrounding the pseudomorphed andalusite porphyroblasts...but decreases the temperatures required to produce new solid phase mineral parageneses (Fig. 8). Thus, water
Journal (article/letter/editorial)
spectacularly preserved (Fig. 2c). Up to 80% of the area of the symplectite is occupied by spinel that occurs...diaspore and cordierite to pinite or fine-grained sericite, but the symplectite textures are still well preserved...points at higher pressures become metastable and new ones appear. On the other hand, our grid is in agreement...calculated for a local composition corresponding to the area surrounding the pseudomorphed andalusite porphyroblasts...but decreases the temperatures required to produce new solid phase mineral parageneses (Fig. 8). Thus, water
Report (volume)
C. Lasaga Geological Laboratory Yale University New Haven, Connecticut 06520 Peter I. Nabelek Dept. of...As in any field of endeavor, we are provided with new questions, thereby dictating future directions of... Goldschmidt's (1911) classic study on the Oslo area of Norway, contact aureoles have provided excellent...circum-Pacific magmatic arc. The intrusives in the shield area of Canada are generalized (metamorphic rocks are...-Diorite Complex of Naran Hill We Dip of Strata THE AREA X Vertical Strata SOUTH OF GWEEBARRA BAY f
Book
955 Massachusetts Avenue, Cambridge, Mass. 02139, USA ' Allen & Unwin (Australia) Ltd, 8 Napier Street...North Sydney, NSW 2060, Australia Allen & Unwin (New Zealand) Ltd in association with the Port Nicholson...Compusales Building, 75 Ghuznee Street, Wellington I, New Zealand First published in 1990 British Library...University Press. Preface This second volume in the new series produced by the Mineralogical Society is concerned...interaction in the north-west Adirondack Mountains, New York State Ian Cartwright & John W. Valley 8. l Introduction
 
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