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• W2014770811 startingPage "135" @default.
• W2014770811 abstract "Heat flow density (HFD) and thermal gradient calculated on the basis of oil well data in the Rif vary from 50 to 90 mW/m2 and from 20 to 50°C/km, respectively. Short-term variations in the west can be attributed to water circulation and lateral heat conductivities contrast along the Pre-Rif thrusting front and at the limits between the main structural units (the Gharb basin, the South Rifian ridges and the Pre-Rif nappe). High HFD and thermal gradient values are determined in the southwest of the study area. This zone extends the central Moroccan massif which is well known by its high thermal manifestations. The External Rif shows a tendency of increasing HFD toward northeastern Morocco and the Alboran Sea. In agreement with the geophysical observations (electrical conductive structures, great negative Bouguer anomaly, shear velocity attenuation, high upper mantle P-velocity), the thermal structure of the External Rif would be a consequence of the presence at subcrustal depths of hot and low-density asthenospheric material overlying a high-velocity lithospheric body beneath the Rif-Betic belt." @default.
• W2014770811 created "2016-06-24" @default.
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• W2014770811 date "1998-02-01" @default.
• W2014770811 modified "2023-09-26" @default.
• W2014770811 title "Heat flow in the westernmost part of the Alpine Mediterranean system (the Rif, Morocco)" @default.
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• W2014770811 doi "https://doi.org/10.1016/s0040-1951(97)00185-6" @default.
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