Syn-rift unconformities punctuating the lower–middle Cambrian transition in the Atlas Rift, Morocco
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The Thaumasia “rift”, Mars – Is It a Rift?
We describe the morphology of a large and complex graben structure in the western Thauma-sia region (the " Thaumasia graben " [1] or TG). We consider possible fault geometries, determine extension , and discuss shortly possible models for its origin. Background: Situated at the western border of the Thaumasia plateau, the TG is one of the most prominent fault-bounded structures on Mars. It is ~...
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ژورنال
عنوان ژورنال: International Journal of Earth Sciences
سال: 2014
ISSN: 1437-3254,1437-3262
DOI: 10.1007/s00531-014-1108-4