C
C. Mark Fanning
Researcher at Australian National University
Publications - 177
Citations - 9733
C. Mark Fanning is an academic researcher from Australian National University. The author has contributed to research in topics: Zircon & Metamorphism. The author has an hindex of 55, co-authored 177 publications receiving 8608 citations.
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Book ChapterDOI
Two Carboniferous Ages: A Comparison of Shrimp Zircon Dating with Conventional Zircon Ages and 40Ar/39Ar Analysis
Journal ArticleDOI
Extraordinary transport and mixing of sediment across Himalayan central Gondwana during the Cambrian–Ordovician
Paul M. Myrow,Nigel C. Hughes,John W. Goodge,C. Mark Fanning,Ian S. Williams,Shanchi （彭善池） Peng,O N Bhargava,S. K. Parcha,Kevin R. Pogue +8 more
TL;DR: In this paper, detrital zircon samples from Cambrian and Lower to Middle Ordovician strata were taken across and along the strike of the Hima-laya from Pakistan to Bhutan (~2000 km).
Journal ArticleDOI
Archean granite-greenstone tectonics at Kolar (South India): Interplay of diapirism and bulk inhomogeneous contraction during juvenile magmatic accretion
TL;DR: A structural study of the Kolar greenstone belt and surrounding granite-gneiss terrains combined with U-Pb dating reveals that the middle and lower crustal tectonoplutonic pattern of the eastern Dharwar craton developed during a major magmatic accretion event between 2550 and 2530 Ma.
Journal ArticleDOI
The lower crust of the Dharwar Craton, Southern India: Patchwork of Archean granulitic domains
Jean-Jacques Peucat,Mudlappa Jayananda,Dominique Chardon,Ramon Capdevila,C. Mark Fanning,Jean-Louis Paquette +5 more
TL;DR: In this article, four lower crustal domains have been identified and investigated across the Neoarchean amphibolite to granulite facies transition zone in the Dharwar Craton.
Journal ArticleDOI
Shrimp U–Pb zircon age evidence for Paleoproterozoic sedimentation and 2.05 Ga syntectonic plutonism in the Nyong Group, South-Western Cameroon: consequences for the Eburnean–Transamazonian belt of NE Brazil and Central Africa
Catherine Lerouge,Alain Cocherie,S.F. Toteu,J. Penaye,Jean-Pierre Milesi,Robert Tchameni,Emmanuel N. Nsifa,C. Mark Fanning,Etienne Deloule +8 more
TL;DR: The Nyong Group of the NW corner of the Congo craton is a metasedimentary and metaplutonic rock unit that underwent a high-grade tectono-metamorphic event at ∼2050-Ma associated with charnockite formation as mentioned in this paper.