Global ETD Search

1	Quantitative analysis of carbonate sandbodies outcrop analog study from an epicontinental basin (Triassic Germany) / Braun, Sascha. January 1900 (has links) (PDF) Tübingen, Univ., Diss., 2003. / Computerdatei im Fernzugriff. Carbonatplattform Südwestdeutschland
2	The miocene carbonates in time and space on- and offshore SW Palawan, Philippines Rehm, Stefan K. Unknown Date (has links) (PDF) University, Diss., 2003--Kiel.
3	Growth and crises of the late Albian, Turonian carbonate platform, west central Jordan integrated stratigraphy and environmental changes / Schulze, Frauke. Unknown Date (has links) (PDF) University, Diss., 2003--Bremen.
4	Diversity, distribution and geochemistry of benthic foraminifera in Holocene lagoons of carbonate platforms (Belize, Central America) Schultz, Sandra. Unknown Date (has links) University, Diss., 2008--Frankfurt (Main). / Dt. Übers. des Hauptsacht.: Diversität, Verbreitung und Geochemie benthischer Foraminiferen in holozänen Lagunen von Karbonatplattformen (Belize, Zentralamerika).
5	Quantitative analysis of carbonate sandbodies outcrop analog study from an epicontinental basin (Triassic Germany) / Braun, Sascha. Unknown Date (has links) (PDF) University, Diss., 2003--Tübingen.
6	Forward numerical modelling of carbonate basins: an ecological approach Clavera-Gispert, Roger 07 December 2016 (has links) (PDF) This thesis presents a new stratigraphic forward numerical model to simulate the carbonate production of marine sedimentary basin through ecological model which is implemented in the SIMSAFADIM-CLASTIC program. This ecological model is based on the Generalized Lotka Voltera equations that model the population evolution of species. These populations are controlled by biological factors (growth rate, carrying capacity and interaction among species), and by the environmental conditions (light, energy of the medium, nutrients, bottom slope and concentration of clastic sediments in suspension) which are combined forming a unique environmental factor that downscale the intrinsic rate of growth. The algorithm to apply in the code uses an explicit Runge-Kutta numerical method of order (4)5 to solve the differential equations formulated in the ecological model. Finally, a 3D visualization output files for the interpretation and analysis are generated using the VTK format. The obtained code has been applied in three sample experiments in order to discuss the possibilities and the limitations of the code. The first example is the model of a theoretical basin. The results are compared with real cases. The second example is an actual basin sited in western Mediterranean Sea. The results are discussed to show the applicability and the limitations of the model. The third example applies several configurations to the Aptian Galve sub-basin (Maestrat Basin, E Iberia), allowing to define the environmental conditions. Prozessbasierte numerische Modellierung Sedimentbecken Carbonat-Produktion sedimentary basin carbonate production ddc:550 Carbonatplattform Schelf Sedimentologie Sedimentation Schelfmeersediment Fazies Beckensediment Carbonatgestein Siliziklastisches Gestein Sedimentationsbecken Meeressediment Modellierung Klastisches Gestein Klastische Sedimentation
7	Forward numerical modelling of carbonate basins: an ecological approach Clavera-Gispert, Roger 01 November 2016 (has links) This thesis presents a new stratigraphic forward numerical model to simulate the carbonate production of marine sedimentary basin through ecological model which is implemented in the SIMSAFADIM-CLASTIC program. This ecological model is based on the Generalized Lotka Voltera equations that model the population evolution of species. These populations are controlled by biological factors (growth rate, carrying capacity and interaction among species), and by the environmental conditions (light, energy of the medium, nutrients, bottom slope and concentration of clastic sediments in suspension) which are combined forming a unique environmental factor that downscale the intrinsic rate of growth. The algorithm to apply in the code uses an explicit Runge-Kutta numerical method of order (4)5 to solve the differential equations formulated in the ecological model. Finally, a 3D visualization output files for the interpretation and analysis are generated using the VTK format. The obtained code has been applied in three sample experiments in order to discuss the possibilities and the limitations of the code. The first example is the model of a theoretical basin. The results are compared with real cases. The second example is an actual basin sited in western Mediterranean Sea. The results are discussed to show the applicability and the limitations of the model. The third example applies several configurations to the Aptian Galve sub-basin (Maestrat Basin, E Iberia), allowing to define the environmental conditions. info:eu-repo/classification/ddc/550 ddc:550

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