Zobrazeno 1 - 10
of 73
pro vyhledávání: '"A. M. Celâl Şengör"'
Publikováno v:
International Journal of Earth Sciences. 111:2017-2035
Autor:
Timothy M Kusky, A M Celâl Şengör
Publikováno v:
National Science Review. 10
We compare and contrast the materials and mechanisms of continental crustal growth in the largest preserved regions of Phanerozoic and Archean juvenile additions to the crust, to test for similarities or differences in the formation of continents thr
Publikováno v:
Mediterranean Geoscience Reviews. 3:399-401
Autor:
A. M. Celâl Şengör
Publikováno v:
International Journal of Earth Sciences. 110:759-765
The great German paleontologist Walter Georg Kuhne (1911–1991) published a book in 1979 with the Title Palaontologie und dialektischer Materialismus (Palaeontology and Dialectic Materialism). This inapposite title is very far from reflecting the co
Autor:
Müge Yazıcı, A. M. Celâl Şengör
Publikováno v:
Mediterranean Geoscience Reviews. 2:327-339
The neotectonics of Turkey comprises a time slice since about the end of the Oligocene and has been dominated by the shortening of Eastern Turkey, which created the Turkish–Iranian high plateau, extension in western Turkey, which created the Aegean
Autor:
A. M. Celâl Şengör, Paul K. Byrne, Richard Ghail, Christian Klimczak, Martha S. Gilmore, Sara Khawja, Sean C. Solomon, David A. Senske, Jennifer L. Whitten, Richard E. Ernst
Publikováno v:
Geology. 49:81-85
Tesserae on Venus are locally the stratigraphically oldest units preserved on the planet. These regions are characterized by pervasive tectonic deformation including normal faults, grabens, thrust faults, and folds. In multiple tesserae, sets of (oft
Autor:
A. M. Celâl Şengör
Publikováno v:
Alexander von Humboldt ISBN: 9783030940072
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6953ca6c147be6ab9350d27ebbb1095a
https://doi.org/10.1007/978-3-030-94008-9_11
https://doi.org/10.1007/978-3-030-94008-9_11
Publikováno v:
Canadian Journal of Earth Sciences. 56:1144-1162
We discuss the structure of the present Hellenic subduction zone. We show that the present Hellenic subduction zone was formed at about 15 Ma when it started to consume the Mediterranean lithosphere and to form the large accretionary wedge that cover
Publikováno v:
Canadian Journal of Earth Sciences. 56:1119-1143
We identify long transform faults that frame the eastern Mediterranean Sea and that were active during Jurassic and probably the Early Cretaceous, during the opening of the central Atlantic Ocean. We show that the African margin of the eastern Medite
Autor:
A. M. Celâl Şengör
Publikováno v:
Canadian Journal of Earth Sciences. 56:xi-xiv
Observations are to test hypotheses and without hypotheses there can be no usable observations. Geology students should be taught to be independent, bold, imaginative thinkers before they become assiduous observers.