Petrogenesis of high-Mg andesites from the Proterozoic Shillong Basin, Northeast India: evidence for continuation of the Central Indian Tectonic Zone to the Assam-Meghalaya Gneissic Complex and its implications for the Columbia supercontinent reconstruction
Author:
Affiliation:
1. Department of Geology, Cotton University, Guwahati, Assam, India
2. Geochronology Lab, Inter University Accelerator Centre, New Delhi, India
3. Department of Geology, University of Delhi, Delhi, India
Funder
Department of Science and Technology, India
Science and Engineering Research Board
University Grants Commission
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206814.2023.2209806
Reference102 articles.
1. The Nature of Mesoproterozoic Central Indian Tectonic Zone with Exhumed and Reworked Older Granulites
2. Petrogenetic evolution of late Cenozoic, post-collision volcanism in western Anatolia, Turkey
3. Determination of rare earth elements in Japanese rock standards by inductively coupled plasma mass spectrometry;Balaram V.;Atomic Spectroscopy,1990
4. Geochemical constraints on the petrogenesis of mafic rocks (metadolerites) from the Proterozoic Shillong Basin, Northeast India: implications for growth of the Greater Indian Landmass
5. ∼1.6 Ga ultrahigh-temperature granulite metamorphism in the Central Indian Tectonic Zone: insights from metamorphic reaction history, geothermobarometry and monazite chemical ages
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