Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-10T07:13:46.553Z Has data issue: false hasContentIssue false

A metamorphosed pyroxenite at Nero Hill, Central Tanzania

Published online by Cambridge University Press:  05 July 2018

H. W. Haslam
Affiliation:
Institute of Geological Sciences, 64-78 Gray's Inn Road, London, W.C. 1, formerly Mineral Resources Division, Tanzania
B. G. Walker
Affiliation:
Mineral Resources Division, P.O. Box 903, Dodoma, Tanzania

Summary

The pyroxenite of Nero Hill has been metamorphosed under relatively low water pressure at the centre and higher water pressure at the margins. Thus a central pyroxenite consisting of diopside, hypersthene, oligoclase, garnet, and a little hornblende grades outward into a hornblende-cummingtonite amphibolite.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1971

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

Eskola, (P.), 1950. Amer. Min. 35, 728.34 [M.A. 11-330].Google Scholar
Grover, (J.E.) and Orville, (P.M.), 1969. Geochimica Acta. 33, 205.26 [M.A. 69-2151.CrossRefGoogle Scholar
Klein, (C.), 1968. Journ. Petrology. 9, 281.330 [M.A. 69-325z].CrossRefGoogle Scholar
Kranck, (S.H.), 1961. Ibid. 2, 150 [M.A. 16-564].Google Scholar
Learce, (B.E.), 1968. Geol. Soc. Amer. Special Paper 98 [M.A. 69-3243].Google Scholar
Walker, (B.G.), 1/125 ooo scale geol. map Tanzania, 1st edn, Q.D.S. to5, Busi (in preparation).Google Scholar
Wafters, (W.A.), 1959. N.Z. Journ. Geol. Geophys. 2, 548.56 [M.A. 14-285].Google Scholar