Геолого-геоморфологическое развитие Притуманганья в кайнозое и его угленосность (Юг Дальнего Востока)
Аннотация
Geological-geomorphological development of Tumangan river basin during Cenozoic period may be divided into four stages: Paleocene-Eocene, Eocene-Oligocene; Miocene and Pliocene-Quaternary. All stages had similar consequences of events: fracture effusion of basalt, terrigenous sedimentation, effusion of acid/intermediate lavas, stratigraphic discontinuations. Coal accumulation happened in Eocene and Miocene. In Late Pliocene-Quaternary time the sedimentation stopped, the basin of Japan Sea expanded, differentiated tectonic movements took place and three geomorphological levels were formed.
Рецензия
Для цитирования:
Тащи С.М., Аблаев А.Г. Геолого-геоморфологическое развитие Притуманганья в кайнозое и его угленосность (Юг Дальнего Востока). Геоморфология и палеогеография. 1999;(1):103-108.
For citation:
Taschi S.N., Ablayev A.G. Geologic-geomorphologic development of Pritumanganie (the southern part of Far East) during Cenozoic period and its coal-bearing properties. Geomorfologiya i Paleogeografiya. 1999;(1):103-108.
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