Amphibolite

Results: 196



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31DUKE GEOLOGICAL LABORATORY

DUKE GEOLOGICAL LABORATORY

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Source URL: dukelabs.com

Language: English - Date: 2010-10-15 12:44:06
32J. metamorphic Geol., 1997, 15, Petrological significance of prograde homogenization of growth zoning in garnet: an example from the Llano Uplift W. CARLSON AND E. SCHWARZE* Department of Geological Sciences, U

J. metamorphic Geol., 1997, 15, Petrological significance of prograde homogenization of growth zoning in garnet: an example from the Llano Uplift W. CARLSON AND E. SCHWARZE* Department of Geological Sciences, U

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Source URL: www.geo.utexas.edu

Language: English - Date: 2009-07-13 14:29:14
33High-pressure metamorphism during the Llano orogeny inferred from Proterozoic eclogite remnants Amy Wilkerson, William D. Carlson, Douglas Smith Department of Geological Sciences, University of Texas, Austin, Texas 78713

High-pressure metamorphism during the Llano orogeny inferred from Proterozoic eclogite remnants Amy Wilkerson, William D. Carlson, Douglas Smith Department of Geological Sciences, University of Texas, Austin, Texas 78713

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Source URL: www.geo.utexas.edu

Language: English - Date: 2009-07-13 14:29:13
34Journal of the Czech Geological Society 48/1–High-K Gabbros Related to the durbachites (Jihlava Massif, Moldanubian Zone)

Journal of the Czech Geological Society 48/1–High-K Gabbros Related to the durbachites (Jihlava Massif, Moldanubian Zone)

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Source URL: www.jgeosci.org

Language: English - Date: 2006-02-27 18:46:52
35Journal of the Czech Geological Society 48/1–High-K Gabbros Related to the durbachites (Jihlava Massif, Moldanubian Zone)

Journal of the Czech Geological Society 48/1–High-K Gabbros Related to the durbachites (Jihlava Massif, Moldanubian Zone)

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Source URL: www.ipe.muni.cz

Language: English - Date: 2012-06-21 13:37:40
36Microsoft Word - Physics and Chemistry of the Earth

Microsoft Word - Physics and Chemistry of the Earth

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Source URL: www.geol.umd.edu

Language: English - Date: 2014-03-24 11:03:41
37quence have been affected by low-grade (greenschist) recrystallization associated with the early Andean strains. The highest grade metamorphic rocks (upper amphibolite facies), and local migmatites, are found in close pr

quence have been affected by low-grade (greenschist) recrystallization associated with the early Andean strains. The highest grade metamorphic rocks (upper amphibolite facies), and local migmatites, are found in close pr

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 03:29:59
38Field study of orbicular rocks in Taylor Valley, southern Victoria Land* sequent petrographic and chemical analyses. The primary purposes of our research are (1) to elucidate the mechanism(s) by which the orbicular rocks

Field study of orbicular rocks in Taylor Valley, southern Victoria Land* sequent petrographic and chemical analyses. The primary purposes of our research are (1) to elucidate the mechanism(s) by which the orbicular rocks

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 06:14:24
39each site. The return of these materials, along with rock cores drilled from outcrops and boulders, and their laboratory analysis, constitute the principal activity of this project. Exposures will range from 1 year to as

each site. The return of these materials, along with rock cores drilled from outcrops and boulders, and their laboratory analysis, constitute the principal activity of this project. Exposures will range from 1 year to as

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 04:01:02
40lengths of interest (>15 kilometers). The pressure altimetry proved unnecessary except to connect the radar data across the bergs and over the grounded ice shelf. Because the radar is considerably more accurate than the

lengths of interest (>15 kilometers). The pressure altimetry proved unnecessary except to connect the radar data across the bergs and over the grounded ice shelf. Because the radar is considerably more accurate than the

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 07:07:04