摘要
Mongolia is located within the Central Asian Orogenic Belt.The belt is consist of numerous tectonic blocks or terranes,which resulted from collisions during the Early Paleozoic(Caledonian orogeny),Late Paleozoic(Hercynian orogeny) and partly in Early Mesozoic(Indosinian orogeny)(Seng r et al.,1993;Heubeck,2001;Badarch et al.,2003).These collisions had a profound effect on the coal-bearing sedimentary basins in Carboniferous,Permian,Jurassic and Cretaceous periods of Mongolia.A total of more than 200 coal occurrences and deposits are known,of which about 70 have been explored.
Mongolia is located within the Central Asian Orogenic Belt.The belt is consist of numerous tectonic blocks or terranes,which resulted from collisions during the Early Paleozoic(Caledonian orogeny),Late Paleozoic(Hercynian orogeny) and partly in Early Mesozoic(Indosinian orogeny)(Seng r et al.,1993;Heubeck,2001;Badarch et al.,2003).These collisions had a profound effect on the coal-bearing sedimentary basins in Carboniferous,Permian,Jurassic and Cretaceous periods of Mongolia.A total of more than 200 coal occurrences and deposits are known,of which about 70 have been explored.
出处
《地球学报》
EI
CAS
CSCD
北大核心
2012年第S1期43-44,共2页
Acta Geoscientica Sinica
