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dc.contributor.advisorRamírez-Martínez, Wilson R.
dc.contributor.authorTorres-Vega, María del C.
dc.date.accessioned2017-12-08T13:52:00Z
dc.date.available2017-12-08T13:52:00Z
dc.date.issued2009-12
dc.identifier.urihttps://hdl.handle.net/20.500.11801/105
dc.description.abstractThe north coast Tertiary limestone of Puerto Rico is composed of carbonate rocks that contain the most important aquifer in Puerto Rico. The dolomites of the north coast of Puerto Rico have been studied by González and Ruiz, (1991) by Ramírez, (2000). Both studies suggest mixing zone dolomitization for these dolomites. This study is based on the study of fluid inclusions analysis in the Puerto Rico north coast dolomites to better constrain in environment of precipitation. Fluid inclusions analysis provides direct information on the environments and the temperatures of precipitation. The samples of dolomites analyzed are from the Montebello Member at the Cibao Formations and the Lares Limestone. The temperatures obtained for the fluid inclusions present in Montebello Member at Cibao Formation at depth (510.1) and (420.1) are 0.0 and 0.1 at depth (510.1) that show a small quantity of salt in the samples. Fluid inclusions can be trapped during the process of recrystallization in diagenetic minerals. The inclusions that are present during the process of recrystallization provide the record of the conditions of recrystallization rather that the original precipitation of the mineral. The inclusions in north coast of Puerto Rico indicated the alterations of dolomites in fresh water environments and small quantity of salts zone where the dolomites have been precipitated meteoric-marine mixing zone. Stable isotopic analysis in the same samples was made to help identify the environments of precipitation. The stable isotopic analysis in Garrochales at Barceloneta Quadrangle, Manatí Quadrangle and Lares Limestone and Montebello Member at the Cibao Formation cores indicated alterations in meteoric and marine water.en_US
dc.description.sponsorshipExxonMobilen_US
dc.language.isoenen_US
dc.subjectFluid inclusionsen_US
dc.subjectIsotopic analysisen_US
dc.subjectTertiary dolomitesen_US
dc.subject.lcshDolomite -- Puerto Rico.en_US
dc.subject.lcshRocks, Carbonate -- Puerto Rico.en_US
dc.titleA fluid inclusions study of Puerto Rico tertiary dolomiteen_US
dc.typeThesisen_US
dc.rights.licenseAll rights reserveden_US
dc.rights.holder(c) 2009 María del C. Torres Vegaen_US
dc.contributor.committeeSantos, Hernán
dc.contributor.committeeSherman, Clark
dc.contributor.representativeSantana, Samuel
thesis.degree.levelM.S.en_US
thesis.degree.disciplineGeologyen_US
dc.contributor.collegeCollege of Arts and Sciences - Sciencesen_US
dc.contributor.departmentDepartment of Geologyen_US
dc.description.graduationSemesterFallen_US
dc.description.graduationYear2009en_US


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  • Theses & Dissertations
    Items included under this collection are theses, dissertations, and project reports submitted as a requirement for completing a graduate degree at UPR-Mayagüez.

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