Paleomagnetism of Middle Paleozoic Basites on the Southeastern Flank of the Vilyui Paleorift

Autor:	K. M. Konstantinov, A. A. Yakovlev, M. D. Tomshin, I. K. Konstantinov
Rok vydání:	2019
Předmět:	geography Paleomagnetism geography.geographical_feature_category Rift 010504 meteorology & atmospheric sciences Paleozoic 010502 geochemistry & geophysics 01 natural sciences Devonian Paleontology Craton Earth and Planetary Sciences (miscellaneous) General Earth and Planetary Sciences Clockwise Kimberlite Geology 0105 earth and related environmental sciences Terrane
Zdroj:	Doklady Earth Sciences. 486:695-698
ISSN:	1531-8354 1028-334X
Popis:	The eastern boundary of the Siberian Craton was formed as a result of rifting that split the continent late in the Middle Paleozoic. The paleomagnetic data derived from the Middle Paleozoic kimberlites and basites that were formed in the zone of the dynamic effect of the Vilyui paleorift attest to the clockwise rotation of the Aldan terrane relative to the Angara–Anabar terrane during the post-Late Devonian time. The amount of rotation of the terranes increases gradually eastward and reaches 22° on the eastern flank of the Chara–Sinsk dyke belt.
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_________::0779010e97716744a73a4688ef8c6c30 https://doi.org/10.1134/s1028334x19060163 Zobrazit plný text záznamu Plný text ve formátu PDF Plný text ve formátu HTML
Nepřihlášeným uživatelům se plný text nezobrazuje	K zobrazení výsledku je třeba se přihlásit.