Magnetic properties related to hydrothermal alteration processes at the Escondida porphyry copper deposit, northern Chile
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics,Economic Geology
Link
http://link.springer.com/content/pdf/10.1007/s00126-014-0514-7.pdf
Reference60 articles.
1. Alpers CN, Brimhall GH (1988) Middle Miocene climatic change in the Atacama Desert, northern Chile: evidence from supergene mineralization at La Escondida. Geol Soc Am Bull 100:1640–1656. doi: 10.1130/0016-7606(1988)100<1640:MMCCIT>2.3.CO;2
2. Arancibia ON, Clark AH (1996) Early magnetite-amphibole-plagioclase alteration-mineralization in the Island Copper porphyry copper-gold-molybdenum deposit, British Columbia. Econ Geol 91:402–438. doi: 10.2113/gsecongeo.91.2.402
3. Astudillo N (2008) Mineralogía magnética y paleomagnetismo en los megayacimientos tipo pórfido cuprífero Chuquicamata y El Teniente, Chile. Unpublished PhD thesis, Universidad de Chile, p 306
4. Astudillo N, Roperch P, Townley B, Arriagada C, Maksaev V (2008) Importance of small block rotations in damage zones along transcurrent faults. Evidence from the Chuquicamata open pit, Northern Chile. Tectonophysics 450:1–20. doi: 10.1016/j.tecto.2007.12.008
5. Astudillo N, Roperch P, Townley B, Arriagada C, Chauvin A (2010) Magnetic polarity zonation within El Teniente copper-molybdenum porphyry deposit, central Chile. Miner Deposita 45:23–41. doi: 10.1007/s00126-009-0256-0
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