Tectonics and evolution of the northeastern extremity of the East-Asian Rift Belt
- 作者: Zabrodin V.Y.1
-
隶属关系:
- Kosygin Institute of Tectonics and Geophysics, Far East Branch
- 期: 卷 11, 编号 3 (2017)
- 页面: 155-162
- 栏目: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211245
- DOI: https://doi.org/10.1134/S1819714017030071
- ID: 211245
如何引用文章
详细
The northeastern extremity of the East-Asian Rift Belt is designated as the Priokhotsky Rift, comprising the broadly north–south Torom (750 × 100 km) and Nizhneamursky (450 × 100 km) open faults formed by a system of northeast striking grabens associated with the closure of the Tan-Lu shear system and north–south striking grabens formed in a setting of oblique extension. Infilling of the grabens corresponding to the rift stage proper is the Eocene−Miocene coal-bearing molasse; the fields of the Miocene basalts are also related to it. The grabens of the rift belt are overlain by the Pliocene–Neopleistocene associations of rift basins in the forming plate cover of the Alpine platform.
作者简介
V. Zabrodin
Kosygin Institute of Tectonics and Geophysics, Far East Branch
编辑信件的主要联系方式.
Email: VZabrodin@rambler.ru
俄罗斯联邦, ul. Kim Yu Chena 65, Khabarovsk, 680000
补充文件
