Así, en estas regiones, el flujo de calor calculado varía de 27, 6 ± 4 para el sector costa afuera de Barranquilla en la zona correspondiente al delta del río Magdalena,ģ7,9 ☓,6 y 33,2 ± 5,5 mW/m 2 para el sector costa afuera de la alta Guajira y Guajira central respectivamente y 34,7 ± 9,4 para el sector costa afuera de Cartagena - Golfo de Urabá. En este estudio se determinó el flujo de calor en el área costa afuera que se extiende desde la alta Guajira hasta el golfo de Urabá con un área interpretada de BSR de aproximadamente 18 000 km 2. Este reflector anómalo, el cual se cree que coincide con la base de la zona de estabilidad de la capa de hidratos de gas, permite estimar un rango de valores de flujo de calor a partir de los diagramas de estabilidad de los hidratos y la correspondiente conductividad termal de los sedimentos. El flujo de calor en zonas con presencia de hidratos de gas puede ser determinado teóricamente a partir de la ocurrencia del reflector simulador de fondo (BSR por su sigla en inglés), el cual ha sido detectado en registros de reflexión sísmica adquirida costa afuera del Caribe Colombiano. Keywords: gas hydrate, bottom simulating reflector (BSR), heat transfer, Caribbean area, Colombia. The Cartagena-Gulf of Uraba zone evidences the presence of advection heat loss in the accretionary wedge of the South Caribbean deformation front. The continuous and fast sedimentation rate from the Magdalena River may explain the anomalously low heat flow in the river delta area. The estimated heat flow is relatively low in relation to other continental margins. These results are comparable to heat flow estimates of 30 and 42 mW/m 2 obtained for the south Caribbean by others using alternate methods. The heat flow was found to be 27,6 ± 4 mW/m 2 off the coast of Barranquilla, 37,9 ± 3,6 mW/m2 for northern Guajira, 33,2 ± 5,5 mW/m 2 for the central Guajira and 34,7 ± 9,4 mW/m 2 for the Cartagena –Gulf of Uraba offshore areas. The study area extends from northern Guajira in the north to the Gulf of Uraba in the south, covering some 18 000 km 2.
This anomalous reflector, known to correspond with the base of the Gas Hydrate Stability Zone (GHSZ), can be used to estimate a range of possible values for the local heat flow using the stability field of gas hydrates and the thermal conductivity of the sediments. A Bottom-Simulating Reflector (BSR) has been observed in multichannel seismic data from the Caribbean offshore Colombia. Geothermal heat flow in gas hydrate zones can be determined theoretically from the Bottom-Simulating Reflector. e-mail: S.A – Instituto Colombiano del Petróleo, A.A. ¹Universidad Industrial de Santander, Escuela de Geología, Bucaramanga, Santander, Colombia. Find your Perfect Property in Santo Domingo in the Dominican Republicįrom luxury villas to new apartments, find your perfect property in Santo Domingo in the Dominican Republic with 7th Heaven Properties.HEAT FLOW IN THE COLOMBIAN CARIBBEAN FROM THE BOTTOM SIMULATING REFLECTOR (BSR)įlujo de calor a partir del reflector simulador de fondo (BSR), en el caribe colombiano Whatever your preference, we can introduce you to lots and homes sites both small and large which would be ideal for your future home. Beachfront, lakefront or in the heart of the city? The choice is yours. The first step is to decide on the location. Santo Domingo Land for SaleĪre you considering building the home of your dreams on the island? 7th Heaven Properties also features land for sale in Santo Domingo – the perfect blank canvas to build a custom home. We are also the perfect place to begin your search for apartments and condos for sale in Santo Domingo. From luxury homes to new construction apartments, explore the finest homes for sale in Santo Domingo in the Dominican Republic with 7th Heaven Properties. Our website features villas, houses and homes in Santo Domingo in the Dominican Republic. Browse Our Santo Domingo Real Estate Listingsīrowse our Santo Domingo real estate listings and explore homes, condos and land for sale in Santo Domingo.
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