Analytical/numerical modeling of komatiite lava emplacement and thermal erosion at Perseverance, Western Australia

David Williams, Ross C. Kerr, C. Michael Lesher, Stephen J. Barnes

Research output: Contribution to journalArticle

41 Citations (Scopus)

Abstract

We have applied a thermal-fluid dynamic-geochemical model to investigate the emplacement and erosional potential of Archean komatiite flows at Perseverance, Western Australia. Perseverance has been proposed as a site of large-scale thermal erosion by large-volume komatiite eruption(s), resulting in a 100-150-m-deep lava channel containing one of the world's largest komatiite-hosted Fe-Ni-Cu-(PGE) sulfide deposits. Using constraints based on field, theoretical, and geochemical data, we have modeled the emplacement of a range of flow thicknesses over felsic tuffaceous substrates with various degrees of consolidation and water contents. Thermo-mechanical erosion becomes more effective for substrates that are increasingly unconsolidated and water rich. For thermo-mechanical erosion to be responsible for the formation of the ∼-100-m-deep, concave Perseverance embayment and the highly-contaminated (∼10-20%) Perseverance komatiites, the most likely scenarios require emplacement of thick (e.g. ≥10-30 m), turbulent, channelized liquidus or superheated komatiite lavas over a welded or unconsolidated submarine tuff. Flow distances must have been long (tens to hundreds of kilometers) and flow volumes must have been very high (hundreds to thousands of km3). Lava channels and tubes >110 km long have not been observed on Earth, but are consistent with those formed by low-viscosity lavas on Venus, the Moon, Mars and lo. Flow volumes are consistent with those in continental flood basalt eruptions and oceanic plateau Large Igneous Provinces, and may represent the initial outpourings of komatiite lavas from Archean mantle plume activity.

Original languageEnglish (US)
Pages (from-to)27-55
Number of pages29
JournalJournal of Volcanology and Geothermal Research
Volume110
Issue number1-2
DOIs
StatePublished - Sep 30 2001

Fingerprint

komatiite
lava
erosion
Erosion
emplacement
modeling
volcanic eruptions
Moon
Sulfides
Substrates
Archean
Fluid dynamics
Prostaglandins E
Consolidation
volcanic eruption
Water content
Deposits
substrate
Earth (planet)
large igneous province

Keywords

  • Komatiite
  • Lava emplacement
  • Numerical modelling
  • Perseverance
  • Thermal erosion

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

Analytical/numerical modeling of komatiite lava emplacement and thermal erosion at Perseverance, Western Australia. / Williams, David; Kerr, Ross C.; Lesher, C. Michael; Barnes, Stephen J.

In: Journal of Volcanology and Geothermal Research, Vol. 110, No. 1-2, 30.09.2001, p. 27-55.

Research output: Contribution to journalArticle

Williams, David ; Kerr, Ross C. ; Lesher, C. Michael ; Barnes, Stephen J. / Analytical/numerical modeling of komatiite lava emplacement and thermal erosion at Perseverance, Western Australia. In: Journal of Volcanology and Geothermal Research. 2001 ; Vol. 110, No. 1-2. pp. 27-55.
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