Please use this identifier to cite or link to this item: http://repositorio.ineel.mx/jspui/handle/123456789/131
12-Oct-2013
4. Versión publicada
Conferencia
Titulo
Is there any compositional link between thermal fluids in mexican deep reservoirs?
Identificador del autor Tipo de identificacion Autor
CURPPETER BIRKLE
Descripcion/Resumen
A linear 180-isotopic gradient of 0.43%0 per lOOm is proposed as a temperature and pressure dependent regional trend for the isotopic evolution of deep formation water in Mexican geothermal and oil reservoirs. A similar positive tendency is observed for the mineralization stage of water, whereby gravity-driven separation processes cause the descent of heavy C1-brines. Additionally, local effects cause an individual chemical and isotopic evolution of each reservoir fluid: The Activo Luna, Samaria-Sitio Grande and Pol-Chuc oil field waters are characterized by a wide range, saline to hypersaline NaC1-and NaCaC1-type compositions, formed by variable mixing of two components - glacial meteoric and evaporated seawater.
Area de conocimiento Campo Disciplina Subdisciplina
CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRACIENCIAS DE LA TIERRA Y DEL ESPACIOGEOLOGÍAENERGÍA Y PROCESOS GEOTÉRMICOS
Audiencia
Público en general
Materias
-
Acceso Abierto
Inglés

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