C
Carla Müller
Researcher at Goethe University Frankfurt
Publications - 47
Citations - 2963
Carla Müller is an academic researcher from Goethe University Frankfurt. The author has contributed to research in topics: Cenozoic & Cretaceous. The author has an hindex of 23, co-authored 47 publications receiving 2789 citations. Previous affiliations of Carla Müller include University of Paris.
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History of the Mediterranean salinity crisis
Kenneth J. Hsü,Lucien Montadert,Daniel Bernoulli,Maria Bianca Cita,Albert Erickson,Robert E. Garrison,Robert B. Kidd,F. Melieres,Carla Müller,Ramil Wright +9 more
TL;DR: In this article, a history of geodynamic evolution of the Mediterranean leading to the salinity crisis is outlined, based on the 'desiccated deep-basin model' and an accurate portrayal of the crisis is presented.
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Back Arc Extension in the Okinawa Trough
Jean-Claude Sibuet,Jean Letouzey,Florence Barbier,Jacques Charvet,Jean Paul Foucher,Thomas W. C. Hilde,Masaaki Kimura,Ling-Yun Chiao,Bruno Marsset,Carla Müller,J. F. Stephan +10 more
TL;DR: In this paper, the authors suggest that the oblique resisting force applied to the edge of the overriding plate engenders the development of en echelon extensional features within and to the arc with respect to the Okinawa Trough.
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Structural evolution of the Kopeh Dagh fold-and-thrust belt (NE Iran) and interactions with the South Caspian Sea Basin and Amu Darya Basin
Alexandra Robert,Alexandra Robert,Jean Letouzey,Mohammad Ali Kavoosi,S. Sherkati,Carla Müller,Jaume Vergés,Abdollah Aghababaei +7 more
TL;DR: In this article, a detailed stratigraphic and structural study of the Kopeh Dagh fold-and-thrust belt in NE Iran is presented, which is an investigation of the complex polyphased tectonic history of this belt and its links with the adjacent South Caspian Sea and Amu Darya basins.
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Neogene arc-continent collision in Sabah, Northern Borneo (Malaysia)—Reply
TL;DR: The Neogene evolution of Sabah can be interpreted in terms of an arc-continent collision initiated during early Middle Miocene time and followed by intraplate shortening, the latter being active in this area at the present day as mentioned in this paper.
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Organic-rich sedimentation at the Cenomanian-Turonian boundary in oceanic and coastal basins in the North Atlantic and Tethys
TL;DR: In this paper, the authors show that organic-rich sediments have a widespread geographical distribution during the period from Upper Cenomanian to Middle Turonian, and that the organogenic accumulation is distributed according to various trends.