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Mongolia has complicated tectonic and structural geology, belonging to the Mongolian-Okhotsk Mobile Zone, between the Siberian Platform and Chinese Platform.The basement rocks formed during the Paleozoic in the Precambrian as Riphean age ophiolite formations experienced rifting from 1.7 to 1.6 billion years ago and again around 800 million years ago.
Pages in category "Geology of Mongolia" The following 4 pages are in this category, out of 4 total. This list may not reflect recent changes. ...
Pages in category "Geologic formations of Mongolia" The following 24 pages are in this category, out of 24 total. This list may not reflect recent changes. A.
Geology of Mongolia (7 C, 4 P) Grasslands of Mongolia (1 P) H. Historical geography of Mongolia (1 C, 3 P) L. Landforms of Mongolia (14 C, 2 P) Landmarks in Mongolia ...
The Argun terrane is a rock unit in Transbaikalia and Mongolia, located in the Mongol-Okhotsk Fold Belt. It has been suggested that it formed part of the palaeocontinent Amuria . [ 1 ] It is connected to the metamorphic complexes of the Siberian craton in the northern region, which is characterized by a narrow strip of mylonites. [ 1 ]
Fossil localities in Mongolia. From C to D, mainly Bayan Shireh locations The Bayan Shireh Formation (also known as Baynshiree/Baynshire , Baynshirenskaya Svita or Baysheen Shireh ) is a geological formation in Mongolia , that dates to the Cretaceous period.
Taryatu-Chulutu (Mongolian: Тариатын чулуут, romanized: tariatyn chuluut, "rocks of Tariat") is a volcanic field in Mongolia. It is part of a volcanic area in Central Asia in the Hangai range that may be linked to the rifting of the Lake Baikal Rift. The field itself is located within the valleys of the Chuluut and Suman rivers.
Mongolia is a landlocked country in East Asia, located between China and Russia. The terrain is one of mountains and rolling plateaus , with a high degree of relief. [ 2 ] The total land area of Mongolia is 1,564,116 square kilometres. [ 3 ]