KUFRA BASIN PDF

This chapter discusses that the present-day shape of both Murzuq and Kufra basins reflects a Variscan and Mesozoic overprint on an older structural relief. The present work is designed to study the sedimentary cover of part of the Kufra Basin by means of potential field analyses and modeling. The basin has been. Research objectives and the reports of the Kufra Basin Project at CASP, Cambridge, UK.

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To view the data for individual basins, select a basin from the dropdown menu below or click the basin name in the overview table.

This will open a separate page with detailed maps. Click here to return to the regional overview page. This page bundles the available data for the Al Kufra Basin in the Africa. Kufrq images are hyperlinks and will open up a separate window with a high resolution PDF image of the map.

The basin data is derived from a lower resolution grid which has been upsampled using GMT. This could have introduced an accuracy which is beyond the original data resolution.

The basin cross section is automatically generated using the available crustal structure data sets.

Khufra Basin – SEPM Strata

Sometimes the data labels are not plotted correctly, depending on the length of the section. The location of the profile is indicated in all maps as dashed-dotted thin black line. For the endpoints of the profile, the two points of a given polygon located farthest away from each other were computed. The dynamic topography history for the basin is derived by tracking the basin centroid.

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The paleo-location for this point is computed using the EarthByte plate kinematic framework rotating the position back in time. The density anomalies are then advected back in time to compute mantle flow with plate motions superimposed using the EarthByte plate rotation framework as surface boundary conditions. The dynamic topography is then derived from the computed density distribution using a free upper boundary. For details regarding the methodology see the following papers: Large-scale lithospheric stress field and topography induced by global mantle circulation.

Effects of latent heat release at phase boundaries on flow in the Earth’s mantle, phase boundary topography and dynamic topography at the Earth’s surface. For explanation to the data source or computation of this grid please follow this link.

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Clicking the image will open a high-res PDF of the map. Units in the statistics table are same as map units.

This basin data is based on interpolated global grids and might contain gridding errors or wrongly interpolated data values. Statistics – Mantle Lid thickness Median Jump to the following kuffa Statistics – Depth of deg isotherm Median Statistics – Mobil isopachs Median 0. Statistics – Plain crustal thickness Median Statistics – Base middle crust Median Statistics – Base lower crust Median Statistics – Total crustal thickness Median Statistics – Base upper crust Median Statistics – Thermal lithospheric thickness Median Statistics – Heatflow Median Statistics – Base hard sediments Median Statistics – Temperature at 50km depth Median Statistics – Laske sediment thickness Median 0.

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Statistics – Lithospheric temperature gradient Median 5. Comments For explanation to the data source or computation of this grid please follow this link. Select data to display: Statistics – Mantle Lid thickness Median. Statistics – Depth of deg isotherm Median. Statistics – Mobil isopachs Median.

Statistics – Plain crustal thickness Median. Statistics – Base middle crust Median. Statistics – Base lower crust Median. Statistics – Total crustal thickness Median. Statistics – Base upper crust Median. Statistics – Thermal lithospheric thickness Median. Statistics – Heatflow Median. Statistics – Base hard sediments Median. Statistics – Temperature at 50km depth Median. Statistics – Laske sediment thickness Median.

Statistics – Lithospheric temperature gradient Median. Statistics – Isostatic correction Median. Statistics – TTS sediment Median. Statistics – Beta Sediment Median. Statistics – Crustal vs lithosph.

Statistics – Predicted elevation Median. Statistics – Beta Crust Median. Statistics – TTS crust Median. Statistics – Differential Beta Median.