STRUCTURAL RECONSTRUCTION OF THE COPPER BASIN AREA, BATTLE MOUNTAIN DISTRICT, NEVADA by David A. Keeler A Prepublication Manuscript Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 2010 1 Structural Reconstruction of the Copper Basin Area, Battle Mountain District, Nevada David A. Keeler* Newmont Mining Corp. P.O. Box 1657, Battle Mountain, NV 89820-1657 and Eric Seedorff Institute for Mineral Resources, Department of Geosciences University of Arizona, Tucson, AZ 85721-0077 *Corresponding author: email,
[email protected] 2 Abstract The Copper Basin area of the Battle Mountain district in north-central Nevada contains a porphyry Mo-Cu deposit (Buckingham), several porphyry-related Au ± Cu deposits in skarn and silica-pyrite bodies (Labrador, Empire, Northern Lights, Surprise, Carissa), and three supergene Cu deposits (Contention, Sweet Marie, Widow). This study uses the results of field mapping, U- Pb dating of zircons from igneous rocks, and structural analysis to assess the age, original geometry, depth of emplacement, and degree of tilting and dismemberment of the Late Cretaceous and Eocene hydrothermal systems the Copper Basin area and the source of the supergene copper. The Copper Basin area consists primarily of clastic rocks of the Cambrian(?) Harmony Formation overlain unconformably by Pennsylvanian-Permian clastic and carbonate rocks of the Antler overlap sequence. On the eastern side of Copper Basin, the Antler overlap sequence is overlain by the late Eocene tuff of Cove Mine, in which the compaction foliation dips 15 to 25° east.