The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite

<p>A large granitic pegmatite near Campo, in southern San Diego County was found to contain several radioactive biotite-rich inclusions. The pegmatite is irregularly zoned, and in general comprises a well defined graphic granite border zone, an irregular wall zone of intergrown quartz and pert...

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Main Author: Foote, Royal Stuart
Format: Others
Language:en
en
Published: 1951
Online Access:https://thesis.library.caltech.edu/5595/1/Foote_rs_1951.pdf
https://thesis.library.caltech.edu/5595/2/Foote_rs_1951_plate.PDF
Foote, Royal Stuart (1951) The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite. Master's thesis, California Institute of Technology. doi:10.7907/R3W3-M749. https://resolver.caltech.edu/CaltechTHESIS:03122010-084454404 <https://resolver.caltech.edu/CaltechTHESIS:03122010-084454404>
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spelling ndltd-CALTECH-oai-thesis.library.caltech.edu-55952021-09-03T05:01:27Z https://thesis.library.caltech.edu/5595/ The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite Foote, Royal Stuart <p>A large granitic pegmatite near Campo, in southern San Diego County was found to contain several radioactive biotite-rich inclusions. The pegmatite is irregularly zoned, and in general comprises a well defined graphic granite border zone, an irregular wall zone of intergrown quartz and perthite, a discontinuous intermediate zone of blocky perthite, and a well developed but somewhat irregular quartz core. The included masses of biotite-rich rock are spatially related to segments of the quartz core and their content of rare-earth minerals may be due in part to this relationship.</p> <p>The inclusions are composed of interlayered biotite books and feldspar plates which form a series of folded and distorted layers that are randomly oriented throughout the inclusion. Separation and analysis of minerals from the inclusion were accomplished by means of cloud-chamber detection, x-ray powder diffraction analyses, and spectrographic analysis. Thorium-bearing monazite was identified as the source of the radio-activity.</p> <p>The rare-earth elements and thorium evidently were concentrated in the late residual fluids of the pegmatite. Pendants or inclusions of apatite-bearing schist are believed to have provided a source of phosphorous for the crystallization of monazite. As an additional result of reaction with the pegmatite solutions, the minerals of the schistose pendant were recrystallized and some mineralogic changes were made as well.</p> 1951 Thesis NonPeerReviewed application/pdf en other https://thesis.library.caltech.edu/5595/1/Foote_rs_1951.pdf application/pdf en other https://thesis.library.caltech.edu/5595/2/Foote_rs_1951_plate.PDF Foote, Royal Stuart (1951) The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite. Master's thesis, California Institute of Technology. doi:10.7907/R3W3-M749. https://resolver.caltech.edu/CaltechTHESIS:03122010-084454404 <https://resolver.caltech.edu/CaltechTHESIS:03122010-084454404> https://resolver.caltech.edu/CaltechTHESIS:03122010-084454404 CaltechTHESIS:03122010-084454404 10.7907/R3W3-M749
collection NDLTD
language en
en
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sources NDLTD
description <p>A large granitic pegmatite near Campo, in southern San Diego County was found to contain several radioactive biotite-rich inclusions. The pegmatite is irregularly zoned, and in general comprises a well defined graphic granite border zone, an irregular wall zone of intergrown quartz and perthite, a discontinuous intermediate zone of blocky perthite, and a well developed but somewhat irregular quartz core. The included masses of biotite-rich rock are spatially related to segments of the quartz core and their content of rare-earth minerals may be due in part to this relationship.</p> <p>The inclusions are composed of interlayered biotite books and feldspar plates which form a series of folded and distorted layers that are randomly oriented throughout the inclusion. Separation and analysis of minerals from the inclusion were accomplished by means of cloud-chamber detection, x-ray powder diffraction analyses, and spectrographic analysis. Thorium-bearing monazite was identified as the source of the radio-activity.</p> <p>The rare-earth elements and thorium evidently were concentrated in the late residual fluids of the pegmatite. Pendants or inclusions of apatite-bearing schist are believed to have provided a source of phosphorous for the crystallization of monazite. As an additional result of reaction with the pegmatite solutions, the minerals of the schistose pendant were recrystallized and some mineralogic changes were made as well.</p>
author Foote, Royal Stuart
spellingShingle Foote, Royal Stuart
The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite
author_facet Foote, Royal Stuart
author_sort Foote, Royal Stuart
title The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite
title_short The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite
title_full The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite
title_fullStr The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite
title_full_unstemmed The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite
title_sort geology of the houser canyon pegmatite with an x-ray analysis of monazite
publishDate 1951
url https://thesis.library.caltech.edu/5595/1/Foote_rs_1951.pdf
https://thesis.library.caltech.edu/5595/2/Foote_rs_1951_plate.PDF
Foote, Royal Stuart (1951) The Geology of the Houser Canyon Pegmatite with an X-Ray Analysis of Monazite. Master's thesis, California Institute of Technology. doi:10.7907/R3W3-M749. https://resolver.caltech.edu/CaltechTHESIS:03122010-084454404 <https://resolver.caltech.edu/CaltechTHESIS:03122010-084454404>
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