AN ACTIVE NEOPROTEROZOIC CONTINENTAL MARGIN OF THE ZAVKHAN MICROCONTINENT (MONGOLIA): ISOTOPIC-GEOCHRONOLOGICAL EVIDENCE-Reference-Cited by-同舟云学术

AN ACTIVE NEOPROTEROZOIC CONTINENTAL MARGIN OF THE ZAVKHAN MICROCONTINENT (MONGOLIA): ISOTOPIC-GEOCHRONOLOGICAL EVIDENCE

Published:2022-12-10 Issue:5 Volume:13 Page:
ISSN:2078-502X
Container-title:Geodynamics & Tectonophysics
language:
Short-container-title:Geodin. tektonofiz.

Author:

Shkolnik S. I.¹,Letnikova E. F.²,Reznitsky L. Z.³

Affiliation:

1. Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences; Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

2. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

3. Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences

Publisher

Institute of Earth's Crust, Siberian Branch of the Russian Academy of Sciences

Subject

Earth-Surface Processes,Geophysics,Geology,Economic Geology

Reference57 articles.

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4. Bold U., Crowley J.L., Smith E.F., Sambuur O., Macdonald F.A., 2016a. Neoproterozoic to Early Paleozoic Tectonic Evolution of the Zavkhan Terrane of Mongolia: Implications for Continental Growth in the Central Asian Orogenic Belt. Lithosphere 8 (6), 729–750. https://doi.org/10.1130/L549.1.

5. Bold U., Smith E.F., Rooney A.D., Bowring S.A., Buchwaldt R., Dudás F.O., Ramezani J., Crowley J.L., Schrag D.P., Macdonald F.A., 2016b. Neoproterozoic Stratigraphy of the Zavkhan Terrane of Mongolia: The Backbone for Cryogenian and Early Ediacaran Chemostratigraphic Records. American Journal of Science 316 (1), 1–63. https://doi.org/10.2475/01.2016.01.

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