Were South India and North China Craton attached during the Paleoproterozoic Nuna Assembly Evidence from geochemical and isotopic investigations from the Khammam Schist Belt Eastern Dharwar Craton

dc.contributor.guideNasipuri,Pritam
dc.coverage.spatial
dc.creator.researcherGanaie,Ab Majeed
dc.date.accessioned2026-02-16T11:10:47Z
dc.date.available2026-02-16T11:10:47Z
dc.date.awarded2025
dc.date.completed2024
dc.date.registered2018
dc.description.abstractnewline
dc.description.note
dc.format.accompanyingmaterialNone
dc.format.dimensions
dc.format.extentv,111
dc.identifier.researcherid
dc.identifier.urihttp://hdl.handle.net/10603/696011
dc.languageEnglish
dc.publisher.institutionEarth and Environmental Sciences
dc.publisher.placeBhopal
dc.publisher.universityIndian Institute of Science Education and Research (IISER) Bhopal
dc.relation
dc.rightsuniversity
dc.source.universityUniversity
dc.subject.keywordEcology and Environment
dc.subject.keywordEnvironmental Sciences
dc.subject.keywordLife Sciences
dc.titleWere South India and North China Craton attached during the Paleoproterozoic Nuna Assembly Evidence from geochemical and isotopic investigations from the Khammam Schist Belt Eastern Dharwar Craton
dc.title.alternative
dc.type.degreePh.D.

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