Genesis of the glaciotectonic thrust-fault complex at Halk Hoved, southern Denmark.
نویسندگان
چکیده
منابع مشابه
fault pattern and estimation of uplift rate along the high zagros thrust fault
(paper pages 133-156) zagros active fold-thrust belt lies on the northern margin of the arabian continental crust it is a young fold-thrust mountain belt currently shortening, thickening and uplifting as a result of the collision of the arabian and iranian plates. rethickening of crust during collisional orogenies could have been carried out by reversal of fault motion along the mesozoic normal...
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ژورنال
عنوان ژورنال: Bulletin of the Geological Society of Denmark
سال: 2012
ISSN: 2245-7070
DOI: 10.37570/bgsd-2012-60-05