A study of unusual diamonds from the George Creek K1 Kimberlite dyke, Colorado

dc.contributor.advisorGurney, John Jen_ZA
dc.contributor.authorChinn, Ingrid Leeen_ZA
dc.date.accessioned2014-10-17T07:29:33Z
dc.date.available2014-10-17T07:29:33Z
dc.date.issued1995en_ZA
dc.description.abstractCathodoluminescence photomicrographs of diamonds from the George Creek Kl (section 28) kimberlite dyke in Colorado reveal complex intergrowth relationships between CO?-free and CO?-bearing diamond growth generations. The distribution of the CO?-bearing diamond in some specimens suggests that this generation is younger than the CO?-free diamond growth generation, although the age relationships are mostly ambiguous. CO?-bearing diamond appears to have crystallized from fluids which invaded fractures and etched embayments in the CO?-free diamond growth generation, which shows evidence of plastic deformation. The CO?-free diamond growth generation commonly exhibits features caused by extreme plastic deformation during mantle residence time. Abundant yellow-green plastic slip planes transect zones of customary blue cathodoluminescence in many diamonds, and raised lamination lines have been recognized on resorption surfaces. The complexity and intensity of surface etch features in most George Creek diamonds, including the CO?-bearing growth generation, suggests that the diamonds were subjected to multiple episodes of etching and resorption. Extensive development of hexagonal and trigonal etch pits resulted from the action of oxidizing CO?-H?O fluids, and some late-stage etching is believed to have occurred in the hypabyssal dyke system prior to kimberlite eruption.en_ZA
dc.identifier.apacitationChinn, I. L. (1995). <i>A study of unusual diamonds from the George Creek K1 Kimberlite dyke, Colorado</i>. (Thesis). University of Cape Town ,Faculty of Science ,Department of Geological Sciences. Retrieved from http://hdl.handle.net/11427/8473en_ZA
dc.identifier.chicagocitationChinn, Ingrid Lee. <i>"A study of unusual diamonds from the George Creek K1 Kimberlite dyke, Colorado."</i> Thesis., University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 1995. http://hdl.handle.net/11427/8473en_ZA
dc.identifier.citationChinn, I. 1995. A study of unusual diamonds from the George Creek K1 Kimberlite dyke, Colorado. University of Cape Town.en_ZA
dc.identifier.ris TY - Thesis / Dissertation AU - Chinn, Ingrid Lee AB - Cathodoluminescence photomicrographs of diamonds from the George Creek Kl (section 28) kimberlite dyke in Colorado reveal complex intergrowth relationships between CO?-free and CO?-bearing diamond growth generations. The distribution of the CO?-bearing diamond in some specimens suggests that this generation is younger than the CO?-free diamond growth generation, although the age relationships are mostly ambiguous. CO?-bearing diamond appears to have crystallized from fluids which invaded fractures and etched embayments in the CO?-free diamond growth generation, which shows evidence of plastic deformation. The CO?-free diamond growth generation commonly exhibits features caused by extreme plastic deformation during mantle residence time. Abundant yellow-green plastic slip planes transect zones of customary blue cathodoluminescence in many diamonds, and raised lamination lines have been recognized on resorption surfaces. The complexity and intensity of surface etch features in most George Creek diamonds, including the CO?-bearing growth generation, suggests that the diamonds were subjected to multiple episodes of etching and resorption. Extensive development of hexagonal and trigonal etch pits resulted from the action of oxidizing CO?-H?O fluids, and some late-stage etching is believed to have occurred in the hypabyssal dyke system prior to kimberlite eruption. DA - 1995 DB - OpenUCT DP - University of Cape Town LK - https://open.uct.ac.za PB - University of Cape Town PY - 1995 T1 - A study of unusual diamonds from the George Creek K1 Kimberlite dyke, Colorado TI - A study of unusual diamonds from the George Creek K1 Kimberlite dyke, Colorado UR - http://hdl.handle.net/11427/8473 ER - en_ZA
dc.identifier.urihttp://hdl.handle.net/11427/8473
dc.identifier.vancouvercitationChinn IL. A study of unusual diamonds from the George Creek K1 Kimberlite dyke, Colorado. [Thesis]. University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 1995 [cited yyyy month dd]. Available from: http://hdl.handle.net/11427/8473en_ZA
dc.language.isoeng
dc.publisher.departmentDepartment of Geological Sciencesen_ZA
dc.publisher.facultyFaculty of Scienceen_ZA
dc.publisher.institutionUniversity of Cape Town
dc.subject.otherGeological Sciencesen_ZA
dc.titleA study of unusual diamonds from the George Creek K1 Kimberlite dyke, Coloradoen_ZA
dc.typeDoctoral Thesis
dc.type.qualificationlevelDoctoral
dc.type.qualificationnamePhDen_ZA
uct.type.filetypeText
uct.type.filetypeImage
uct.type.publicationResearchen_ZA
uct.type.resourceThesisen_ZA
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