Current report on the course “Continental Margin Tectonics and Marine Geodynamics” is intended to highlight the problem of the ocean trench formation of ocean seafloor geomorphological structure in the zones of the continental margin tectonic plates bending. A case study of this essay is morphology of the abyssal ocean trenches and how we can measure and analyze the structure of the ocean floor in the least reachable locations of the world ocean. The report consists of five chapters. The introduction chapter is aimed at understanding the structure of the main geomorphological elements of the continental margin tectonics, as well as the basics of the marine geology are summarized. The second chapter is focused on the studies of th...
Earth’s sea floor is created along great volcanic ridges that spread at rates of a few centimeters p...
The past decade has seen a hyperfast evolution in our knowledge of the processes, provinces, and fea...
Bu çalışmada okyanus tabanının topografyası; derin deniz tabanı ve kıtasal kenarlar olmak üsere iki ...
Current report on the course “Continental Margin Tectonics and Marine Geodynamics” is intended to hi...
The development of high-precision surveying instruments over the last 30 years has made possible the...
The development of high-precision surveying instruments over the last 30 years has made possible the...
The study of the topography and structure of the ocean floor is one of the most important stages in ...
Although only recognized in the middle of the last century, oceanic trenches are among the most spec...
A detailed survey of the Oceanographer transform fault and environs at 35º N, 35ºW has yielded detai...
A detailed survey of the Oceanographer transform fault and environs at 35º N, 35ºW has yielded detai...
A detailed survey of the Oceanographer transform fault and environs at 35º N, 35ºW has yielded detai...
A detailed survey of the Oceanographer transform fault and environs at 35º N, 35ºW has yielded detai...
The study presents the insights of the tectonic development and geological settings of the Atlantic ...
Abstract: During the last 20 years, regional studies on the West Iberia margin and on the former mar...
The past decade has seen a hyperfast evolution in our knowledge of the processes, provinces, and fea...
Earth’s sea floor is created along great volcanic ridges that spread at rates of a few centimeters p...
The past decade has seen a hyperfast evolution in our knowledge of the processes, provinces, and fea...
Bu çalışmada okyanus tabanının topografyası; derin deniz tabanı ve kıtasal kenarlar olmak üsere iki ...
Current report on the course “Continental Margin Tectonics and Marine Geodynamics” is intended to hi...
The development of high-precision surveying instruments over the last 30 years has made possible the...
The development of high-precision surveying instruments over the last 30 years has made possible the...
The study of the topography and structure of the ocean floor is one of the most important stages in ...
Although only recognized in the middle of the last century, oceanic trenches are among the most spec...
A detailed survey of the Oceanographer transform fault and environs at 35º N, 35ºW has yielded detai...
A detailed survey of the Oceanographer transform fault and environs at 35º N, 35ºW has yielded detai...
A detailed survey of the Oceanographer transform fault and environs at 35º N, 35ºW has yielded detai...
A detailed survey of the Oceanographer transform fault and environs at 35º N, 35ºW has yielded detai...
The study presents the insights of the tectonic development and geological settings of the Atlantic ...
Abstract: During the last 20 years, regional studies on the West Iberia margin and on the former mar...
The past decade has seen a hyperfast evolution in our knowledge of the processes, provinces, and fea...
Earth’s sea floor is created along great volcanic ridges that spread at rates of a few centimeters p...
The past decade has seen a hyperfast evolution in our knowledge of the processes, provinces, and fea...
Bu çalışmada okyanus tabanının topografyası; derin deniz tabanı ve kıtasal kenarlar olmak üsere iki ...