4.5 Article

Tectonic restoration of the Precambrian crystalline rocks along the west coast of India: Correlation with eastern Madagascar in East Gondwana

期刊

PRECAMBRIAN RESEARCH
卷 252, 期 -, 页码 191-208

出版社

ELSEVIER
DOI: 10.1016/j.precamres.2014.07.013

关键词

Antongil-Antananarivo; Coorg granulites; Western Dharwar Craton; Monazite geochronology; Bemarivo Belt; Gondwanaland

资金

  1. CSIR-UGC [20-6/2008(ii)EU-IV]
  2. Indian Institute of Technology, Kharagpur (India)

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New structural-mineralogical data and U-Th-total Pb monazite chemical ages in 27 samples in a 430 km long corridor along the west coast of India are combined with existing data to reconstruct the tectonic set up of the Meso/Neoarchean crystalline rocks in the Western Dharwar Craton (WDC). The data helps to delineate two NW-trending Paleoproterozoic ductile shear zones that limit the southern and the northern margins of the WDC. The southern shear zone (metamorphic age: 2.3-2.4 Ga) separates the greenschist facies supracrustal belts (2.5 and 3.3 Ga), foliated granitoids (2.5 and 2.9 Ga) and amphibolite facies anatectic gneisses (>3.0 Ga) of the WDC from the >2.9 Ga granulite facies ortho/para-gneisses of the Coorg Block. This shear zone is correlated with the similar to 2.4 Ga Betsimisaraka suture zone in east-central Madagascar that demarcates the accretion zone between the Antongil Block (approximate to WDC) and the granulite fades lithologies of the Antananarivo domain (approximate to Coorg Block). The northern shear zone system (metamorphic age: 2.2-1.8 Ga) extending NW into Madagascar possibly exists as a hitherto undiscovered tectonic zone forming the basement of the Mesoproterozoic Sahantaha Formation underlying the Neoproterozoic Bemarivo Belt supracrustals in NE Madagascar. Within the WDC, the Meso/Neoproterozoic ages retrieved from poorly-defined margins in monazite are uncommon, dispersed within the craton, and do not define localized zones within the craton. The chemical ages of metamorphic monazites formed at greenschist/amphibolite facies conditions preclude metamorphism-deformation associated with accretion of crustal blocks within the WDC during the Rodinia assembly. (C) 2014 Elsevier B.V. All rights reserved.

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