Constraints on the development of orogenic style gold mineralisation at Mineral de Talca, Coastal Range, central Chile: evidence from a combined structural, mineralogical, S and Pb isotope and geochronological study-Reference-Cited by-同舟云学术

Constraints on the development of orogenic style gold mineralisation at Mineral de Talca, Coastal Range, central Chile: evidence from a combined structural, mineralogical, S and Pb isotope and geochronological study

Published:2014-12-04 Issue:6 Volume:50 Page:675-696
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Firth Emily A.,Holwell David A.,Oliver Nicholas H. S.,Mortensen James K.,Rovardi Matthew P.,Boyce Adrian J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

http://link.springer.com/content/pdf/10.1007/s00126-014-0568-6.pdf

Reference54 articles.

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2. Bierlein FP, Crowe DE (2000) Phanerozoic orogenic lode gold deposits. In: Hagemann SG, Brown PE (eds) Gold in 2000. Reviews in Econ Geol 13. Soc Econ Geologists, Littleton, pp 103–139

3. Carrillo-Rosúa J, Boyce AJ, Morales-Ruano S, Morata D, Roberts S, Munizaga F, Moreno-Rodríguez V (2013) Extremely negative and inhomogeneous sulfur isotope signatures in Cretaceous Chilean Manto type Cu-(Ag) deposits, Coastal Range of Central Chile. Ore Geol Revs 56:13–24

4. Cassidy KF, Groves DI, McNaughton NJ (1998) Late-Archean granitoid-hosted lode-gold deposits, Yilgarn Craton, Western Australia: deposit characteristics, crustal architecture and implications for ore genesis. Ore Geol Revs 13:65–102

5. Chen SF, Libby JW, Greenfield JE, Wyche S, Riganti A (2001) Geometry and kinematics of large arcuate structures formed by impingement of rigid granitoids into greenstone belts during progressive shortening. Geology 29:283–286

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