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This document presents a tribute to the memory of my colleague and friend Abdelkader Sellal, a retired geodesist engineer from the Algerian Institute of Cartography and Remote Sensing. I published a report he had written in 2004 where he had proposed projects concerning the modernization of Algerian Geodesy in particular: - Establishment of a Network of Permanent GPS Stations and a Basic Geodetic Network.- GPS calculations. Re-Adjustment and redefinition of the Algerian national geodetic network using adjustment software.- Definition of a System and a Reference of Altitudes in Algeria.- The Geoid: Studies on the determination of a gravimetric geoid in Algeria. Category: Geophysics
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A summary of the Raman-spectroscopic analysis of rock-samples which I have collected near the Ø 15 x 11 km Anaga Impact Crater on Tenerife, and on other interesting sites on this Island. From the analysed feldspar-samples some samples may show Raman-spectra which indicate (W)-weakly-shocked or (M)-moderately-shocked Feldspar. But these Raman-spectra must be analysed by experts who have the experience to correctly assess such spectra. The Raman-spectra of the feldspar-samples from sites No.: 2, 5, 7, 9 & 58 may indicate shocked minerals. (an explanation to Raman spectra of shocked Alkali-Feldspar: see at page 30 in the Appendix_3). Minerals that were indicated by the Raman-spectroscopic analyses : Labradorite(2); Orthoclase(5); Augite, Titanite, Reyerite, Analcime(7); Annite, Augite(9); Anorthoclase(58) (->samples site No. in () Beside possible shocked minerals or minerals which may indicate an impact event, there definitely is one site on Tenerife that should be examined in more detail, in regards to the described impact event. This is sample-site 58, where an old-rock-island is located inside the large caldera of the Pico del Teide Volcano. This mass of old-rock probably was lifted by the impact or by the later volcano, from the original ancient ocean floor. Other interesting sites are located on the road along the ridge-top of the Anaga-Range, in the Teno-Mountain-Range and on site 10 which also belongs to the old basaltc shield of Tenerife. According to my hypothesis the hot spots which caused the Canary Islands originally were impact sites of large ejecta fragments, which were ejected from the Permian Triassic Impact Crater in the Arctic Sea. And I am sure that these impact sites (hot spots) were produced by the same large-scale secondary impact event (caused by the PTI), which also has formed the "Bay of Lyon Crater" and other secondary-impact-structures in Spain. This large-scale impact event is visible on the Gravity-Anomaly Map of the Canarian Islands. The PT-Impact Event probably formed a large secondary-crater, the hypothetical Ø430x290km Gibraltar-Crater (GIC) (see gravity anomaly map). The oblique (ellipitical) impact-craters indicated on this Gravity-Anomaly-map, offshore of Tenerife, Fuerteventura and Lanzarote, all belong to this impact-event and are located along the hypothetical crater-wall (-rim) of the GIC. A magnetic-anomaly-map of the Atlantic-Ocean-floor south-west of Spain provides indication for this Ø430x290 km Gibraltar Crater. (see the explanation on pages 28 & 29 of my PT-Impact-Hypothesis Part-2. Category: Geophysics
We propose a novel approach for flow simulations in fractured porous media based on an equi-dimensional representation of the fractures and a standard continuous finite element (FE) method. We employ an adaptive mesh refinement strategy to automatically adjust an initial regular mesh to any fracture distribution with a desired accuracy. The proposed approach is easily implementable in any FE software, does not involve the coupling of different discretizations, and provides symmetric and positive definite stiffness matrices. We provide a systematic vali- dation of our method and we show that it can be used to simulate fluid flow for fracture networks of realistic complexity. Category: Geophysics
This document presents a tribute to the memory of my colleague and friend Abdelkader Sellal, a retired geodesist engineer from the Algerian Institute of Cartography and Remote Sensing. I published a report he had written in 2004where he had proposed projects concerning the modernization of Algerian Geodesy in particular :- Establishment of a Network of Permanent GPS Stations and a Basic Geodetic Network.- GPS calculations. Re-Adjustment and redefinition of the Algerian national geodetic network using adjustment software.- Definition of a System and a Reference of Altitudes in Algeria.- The Geoid: Studies on the determination of a gravimetric geoid in Algeria. Category: Geophysics
This document presents a tribute to the memory of my colleague and friend Abdelkader Sellal, a retired geodesist engineer from the Algerian Institute of Cartography and Remote Sensing. I published a report he had written in 2004 where he had proposed projects concerning the modernization of Algerian Geodesy in particular: - Establishment of a Network of Permanent GPS Stations and a Basic Geodetic Network. - GPS calculations. Re-Adjustment and redefinition of the Algerian national geodetic network using adjustment software. - Definition of a System and a Reference of Altitudes in Algeria. - The Geoid: Studies on the determination of a gravimetric geoid in Algeria. Category: Geophysics
Here a summary of the Raman-spectroscopic analysis a of rock-samples which I have collected near the Ø 15 x 11 km Anaga Impact Crater on Tenerife, and on other interesting sites on this Island. From the analysed feldspar-samples some samples may show Raman-spectra which indicate (W)-weakly-shocked or (M)-moderately-shocked Feldspar. But these Raman-spectra must be analysed by experts who have the experience to correctly assess such spectra. The Raman-spectra of the feldspar-samples from sites No.: 2, 5, 7, 9 & 58 may indicate shocked minerals. (an explanation to Raman spectra of shocked Alkali-Feldspar: see at page 30 in the Appendix_3). Minerals that were indicated by the Raman-spectroscopic analyses : Labradorite(2); Orthoclase(5); Augite, Titanite, Reyerite, Analcime(7); Annite, Augite(9); Anorthoclase(58) (->samples site No. in () Beside possible shocked minerals or minerals which may indicate an impact event, there definitely is one site on Tenerife that should be examined in more detail, in regards to the described impact event. This is sample-site 58, where an old-rock-island is located inside the large caldera of the Pico del Teide Volcano. This mass of old-rock probably was lifted by the impact or by the later volcano, from the original ancient ocean floor. Other interesting sites are located on the road along the ridge-top of the Anaga-Range, in the Teno-Mountain-Range and on site 10 which also belongs to the old basaltc shield of Tenerife. According to my hypothesis the hot spots which caused the Canary Islands originally were impact sites of large ejecta fragments, which were ejected from the Permian Triassic Impact Crater in the Arctic Sea. And I am sure that these impact sites (hot spots) were produced by the same large-scale secondary impact event (caused by the PTI), which also has formed the "Bay of Lyon Crater" and other secondary-impact-structures in Spain. This large-scale impact event is visible on the Gravity-Anomaly Map of the Canarian Islands. The PT-Impact Event probably formed a large secondary-crater, the hypothetical Ø430x290km Gibraltar-Crater (GIC) (see gravity anomaly map). The oblique (ellipitical) impact-craters indicated on this Gravity-Anomaly-map, offshore of Tenerife, Fuerteventura and Lanzarote, all belong to this impact-event and are located along the hypothetical crater-wall (-rim) of the GIC. A magnetic-anomaly-map of the Atlantic-Ocean-floor south-west of Spain provides indication for this Ø430x290 km Gibraltar Crater. (see the explanation on pages 28 & 29 of my PT-Impact-Hypothesis Part-2. Category: Geophysics 2ff7e9595c
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