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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.
Mongolia is a landlocked country in East Asia, ... The name Gobi is a Mongol word meaning desert, ... GEOLOGY OF THE KHARKHIRAA UUL, MONGOLIAN ALTAI
The map shows that the Central Asian Orogenic Belt is located at the northern portion of Asia, and can be divided into two major parts, which are Kazakhstan orocline and Tuva-Mongolia orocline. It is bounded by the East Europe Craton, Siberia Craton , Karakum Craton, Tarim Craton, and North China Craton . [ 7 ]
The Ek-tagh or Mongolian Altai, which separates the Khovd basin on the north from the Irtysh basin on the south, is a true border-range, in that it rises in a steep and lofty escarpment from the Dzungarian depression (470–900 m (1,540–2,950 ft)), but descends on the north by a relatively short slope to the plateau (1,150–1,680 m (3,770 ...
Far view of the Flaming Cliffs. The Flaming Cliffs site (also known as Bayanzag (Chinese: 巴彥扎格), Bain-Dzak or Bayn Dzak) [1] (Mongolian: Баянзаг rich in saxaul), with the alternative Mongolian name of Mongolian: Улаан Эрэг (red cliffs), is a region of the Gobi Desert in the Ömnögovi Province of Mongolia, in which important fossil finds have been made.
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. ...
Geology portal; Geological formations of Mongolia. Subcategories. This category has the following 4 subcategories, out of 4 total. ...
The Djadochta formation (sometimes transcribed and also known as Djadokhta, Djadokata, or Dzhadokhtskaya) is a highly fossiliferous geological formation in Central Asia, Gobi Desert, dating from the Late Cretaceous period, about 75 million to 71 million years ago.