Hostname: page-component-586b7cd67f-t8hqh Total loading time: 0 Render date: 2024-11-24T11:56:43.332Z Has data issue: false hasContentIssue false
  • English
  • Français

The release of trace elements and volatiles from crinoidal limestone during thermal decrepitation

Published online by Cambridge University Press:  05 July 2018

A. H. Rankin ,
M. F. Miller  and
J. S. Carter
A. H. Rankin
Affiliation:
Department of Geology, Imperial College, London SW7 2BP
M. F. Miller
Affiliation:
British Geological Survey, Geochemical Division, London WC1X 8NG
J. S. Carter
Affiliation:
Mercury Hydrocarbon Limited, Raheen Industrial Estate, Limerick, Eire
Get access Rights & Permissions [Opens in a new window]

Abstract

A suite of coarsely crystalline samples of crinoidal limestone adjacent to a PbS-CaF2-CaCO3 vein in the North Pennine orefield (Greenhow Rake) was analysed by three independent methods [Inductively Coupled Plasma emission spectroscopy (ICP), Mass Spectrometry (MS) and Gas Chromatography (GC)], in order to determine the nature and origin of trace elements and volatiles released on heating and thermal decrepitation, to establish whether fluid inclusions from the host limestone differed in composition from those within the vein, and to assess the value of the results obtained for mineral exploration. The ICP method gave reproducible results for Ca, Na and K, and significant values for Pb and Zn. Na and K correlate with H2O levels determined by MS/volumetric analysis, suggesting their coexistence within fluid inclusions. No such correlation was found for Pb and Zn, suggesting that these elements were derived by volatilisation, perhaps from traces of galena and sphalerite. Methane showed no correlation with H2O and a source other than aqueous fluid inclusions is thought probable for this volatile.

The vein calcite showed much lower K/Na fluid ratios (0.05 cf 0.1–0.2), than the limestones. The limestone-hosted fluids occur predominantly in crinoid ossicles and are believed to represent early pre-mineralisation fluids, unrelated to those associated with veining. Combined ICP and MS techniques may be of value in investigating samples where fluid inclusions are too small for microthermometric and optical analysis.

Keywords

limestonecrinodalthermal decrepitationinductively coupled plasma emission spectroscopymass spectrometrygas chromatography
Type
Mineralogy and petroleum genesis
Information
Mineralogical Magazine , Volume 51 , Issue 362 , October 1987 , pp. 517 - 525
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1987

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Alderton, D.H. M., Thompson, M.J., Rankin, A.H. and Chryssoulis, S.L. (1982) Chem. Geol. 37, 203-13.CrossRefGoogle Scholar
Burruss, R.C. (1981) In Mineral. Assoc. Canada Handbook 6, 138-58 (Hollister, L.S. and Crawford, M.L.,eds.).Google Scholar
Carter, J.S. and Cazalet, P.C. D. (1984) In Prospecting in areas of glaciated terrains. Spec. Publ. Inst. Mining Metalk 11-20.Google Scholar
Chryssoulis, S.L. (1983) Ph.D. Thesis, University of London (Imperial College).Google Scholar
Dunham, K.C. and Stubblefield, C.J. (1944) Q.J. Geol. Soc. Lon. 50, 209-68.CrossRefGoogle Scholar
Dunham, K.C. and Stubblefield, C.J.and Wilson, A.A. (1985) Geology of the North Pennine Orefield 2, Econ. Mere. Brit. Geol. Surv. 247 ppGoogle Scholar
Greenwood, D. and Smith, F.W. (1977) Trans. Inst. Mining Metall. 86, B181–90.Google Scholar
Jones, E. (1986) Ph.D. Thesis, University of London (Imperial College).Google Scholar
Rankin, A.H. and Alderton, D.H.M. (1985) In High Heat Production Granites; Hydrothermal Circulation and Ore Genesis. Spec. Publ. Inst. Mining Metall. 287-300.Google Scholar
Rankin, A.H., Alderton, D.H.M., Thompson, M. and Goulter, J.E. (1982) Mineral. Mag. 46, 179-86.CrossRefGoogle Scholar
Roedder, E. (1977) Econ. Geol. 72, 503-25.Google Scholar
Roedder, E. (1984) Reviews in Mineralogy 12, Mineral. Soc. America.CrossRefGoogle Scholar
Rogers, P.J. (1978) Trans. Inst. Mining Metall. 87, B125-31.Google Scholar
Sawkins, F.J. (1966) Econ. Geol. 61, 385-99.CrossRefGoogle Scholar
Shepherd, T.J., Rankin, A.H. and Alderton, D.H. M. (1985) A practical guide to fluid inclusion studies. Blackie and Sons (Glasgow), 239 ppGoogle Scholar
Small, A.T. (1978) Trans. Inst. Mining Metall. 87, B9-14.Google Scholar
Thompson, M., Rankin, A.H., Walton, S.J., Halls, C. and Foo, B.N. (1980) Chem. Geol. 30, 121-33.CrossRefGoogle Scholar
Yermakov, N.P. (1967) Internat. Geol. Rev. 9, 947-56 [Translated from Sovetskay Geologiya 9, 77-90,1966 (in Russian)].Google Scholar