Lamprophyre

Results: 49



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1IRRRB Diamondsindd

IRRRB Diamondsindd

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Source URL: files.dnr.state.mn.us

Language: English - Date: 2016-06-20 07:42:15
2Precambrian Research–305 www.elsevier.com/locate/precamres Petrology and geochemistry of late-stage intrusions of the A-type, mid-Proterozoic Pikes Peak batholith (Central Colorado, USA): implications for

Precambrian Research–305 www.elsevier.com/locate/precamres Petrology and geochemistry of late-stage intrusions of the A-type, mid-Proterozoic Pikes Peak batholith (Central Colorado, USA): implications for

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Source URL: www.bowdoin.edu

Language: English - Date: 2016-06-30 14:55:30
3A Refresher Course on Crystallography, Mineralogy, Igneous Petrology and Thermodynamics Report: A Refresher course on Crystallography, Mineralogy, Igneous Petrology and Thermodynamics was organized by Alok K. Gupta (Alla

A Refresher Course on Crystallography, Mineralogy, Igneous Petrology and Thermodynamics Report: A Refresher course on Crystallography, Mineralogy, Igneous Petrology and Thermodynamics was organized by Alok K. Gupta (Alla

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Source URL: web-japps.ias.ac.in

Language: English - Date: 2015-02-19 05:45:07
4

PDF Document

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Source URL: www.the-conference.com

Language: English - Date: 2009-11-05 06:45:44
5Goldschmidt Conference Abstracts  An experimental study of minettes and associated mica-clinopyroxenite xenoliths from the Milk River area, Southern Alberta, Canada

Goldschmidt Conference Abstracts An experimental study of minettes and associated mica-clinopyroxenite xenoliths from the Milk River area, Southern Alberta, Canada

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Source URL: goldschmidt.info

Language: English - Date: 2011-09-22 15:07:25
62074  Goldschmidt Conference Abstracts LA-ICPMS U-Pb ages of Paleo- and Mesoproterozoic granites in Bolivia

2074 Goldschmidt Conference Abstracts LA-ICPMS U-Pb ages of Paleo- and Mesoproterozoic granites in Bolivia

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Source URL: goldschmidt.info

Language: English - Date: 2011-09-22 14:29:22
7Goldschmidt 2000 September 3rd–8th, 2000 Oxford, UK. Journal of Conference Abstracts Volume 5(2), 226

Goldschmidt 2000 September 3rd–8th, 2000 Oxford, UK. Journal of Conference Abstracts Volume 5(2), 226

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Source URL: www.the-conference.com

Language: English - Date: 2009-11-05 06:19:01
8GeoLinesual liquids and partly also condensed fluid-phase solutes, and (3) globulae of immiscible melts rich in felsic components and volatiles. The first and second types are common, whereas the third one is

GeoLinesual liquids and partly also condensed fluid-phase solutes, and (3) globulae of immiscible melts rich in felsic components and volatiles. The first and second types are common, whereas the third one is

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Source URL: geolines.gli.cas.cz

Language: English - Date: 2006-03-13 15:37:30
9DIFFERENTIATION OF A BASIC MAGMA Empty the envelope and turn all the pieces of card printed side upwards but randomly arranged and on the part of the desk away from you. The first crystals formed in a cooling basic magma

DIFFERENTIATION OF A BASIC MAGMA Empty the envelope and turn all the pieces of card printed side upwards but randomly arranged and on the part of the desk away from you. The first crystals formed in a cooling basic magma

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Source URL: www.earth-science-activities.co.uk

Language: English - Date: 2013-08-18 13:18:44
10GeoLinesual liquids and partly also condensed fluid-phase solutes, and (3) globulae of immiscible melts rich in felsic components and volatiles. The first and second types are common, whereas the third one is

GeoLinesual liquids and partly also condensed fluid-phase solutes, and (3) globulae of immiscible melts rich in felsic components and volatiles. The first and second types are common, whereas the third one is

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Source URL: www.ipe.muni.cz

Language: English - Date: 2012-06-21 13:37:43