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Lithocaps - characteristics, origins and significance for porphyry and epithermal exploration
conference contribution
posted on 2023-05-23, 12:58 authored by David CookeDavid Cooke, Noel WhiteNoel White, Lejun ZhangLejun Zhang, Chang, Z, Chen, HLithocaps are subsurface, broadly stratabound alteration domains that are laterally and vertically extensive. They form when acidic magmatic-hydrothermal fluids react with wallrocks during ascent towards the paleosurface. Although lithocaps typically have steeply-dipping structural roots, there is a significant component of lateral fluid flow involved in lithocap formation, either through permeable aquifers and/or a well-developed fracture mesh. Lithocaps can have lateral dimensions greater than 10 km and thicknesses of more than 1 km. In ancient settings, partially eroded lithocaps are typically exposed as silicified ridges and cliffs. These features do not mark the original paleosurface – instead they are erosional remnants of what was once an extensive subsurface alteration domain that may have been capped by low temperature argillic- and/or propylitic-altered rocks. High sulfidation state mineralisation typically occurs in silicicaltered rocks within lithocaps, either as stratabound replacements, veins and/or breccia cement. The quartz-rich mineralized domains can produce a resistivity high. Pyrite is ubiquitous in lithocaps prior to weathering, and can yield complicated chargeability responses, some of which may be associated with mineralization. The alteration assemblages are invariably magnetite-destructive, and can obscure the magnetic signature of an underlying porphyry deposit. Combining SWIR and whole rock geochemistry can provide effective vectoring tools within lithocaps.
Funding
Australian Research Council
AMIRA International Ltd
BHP Billiton Ltd
Newcrest Mining Limited
History
Publication title
Proceedings of the 14th SGA Biennial Meeting: Mineral Resources to DiscoverEditors
P Mercier-Langevin, B Dube, M Bardoux, P-S Ross, C DionPagination
291-294ISBN
9782981689801Department/School
School of Natural SciencesPublisher
Society for Geology Applied to Mineral DepositsPlace of publication
SwitzerlandEvent title
14th SGA Biennial MeetingEvent Venue
Quebec City, CanadaDate of Event (Start Date)
2017-08-20Date of Event (End Date)
2017-08-23Rights statement
Copyright 2017 Society for Geology Applied to Mineral DepositsRepository Status
- Restricted