Journal article

Evolution of natrocarbonatite from a wollastonite nephelinite parent: Evidence from the June, 1993 eruption of Oldoinyo Lengai, Tanzania

Abstract:: Lapilli and unusually thick, high viscosity lavas extruded from Oldoinyo Lengai in June, 1993 are composed of crystal-rich natrocarbonatite containing a small proportion of porphyritic silicate spheroids. The silicate spheroids are of wollastonite nephelinite mineralogy, but they also contain natrocarbonatite mineral grains and aggregates (a) in glass inclusions within nepheline and pyroxene phenocrysts, and (b) within the fine-grained silicate groundmass of the spheroids. The chemical relati...
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Publication status:: Published

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APA Style

Dawson, J., Pyle, D., & Pinkerton, H. (1996). Evolution of natrocarbonatite from a wollastonite nephelinite parent: Evidence from the June, 1993 eruption of Oldoinyo Lengai, Tanzania. JOURNAL OF GEOLOGY, 104(1), 41–54.

MLA Style

Dawson, J., et al. “Evolution of Natrocarbonatite from a Wollastonite Nephelinite Parent: Evidence from the June, 1993 Eruption of Oldoinyo Lengai, Tanzania.” JOURNAL OF GEOLOGY, vol. 104, no. 1, 1996, pp. 41–54.

Chicago Style

Dawson, J, D Pyle, and H Pinkerton. 1996. “Evolution of Natrocarbonatite from a Wollastonite Nephelinite Parent: Evidence from the June, 1993 Eruption of Oldoinyo Lengai, Tanzania.” JOURNAL OF GEOLOGY 104 (1): 41–54.
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Publisher copy:: 10.1086/629800

Authors

+ Dawson, J More by this author

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Author

+ Pyle, D More by this author

Institution:

University of Oxford

Division:

MPLS

Department:

Earth Sciences

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Author

+ Pinkerton, H More by this author

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Author

Bibliographic Details

Journal:: JOURNAL OF GEOLOGY More from this journal
Volume:: 104
Issue:: 1
Pages:: 41-54
Publication date:: 1996-01-01
DOI:: 10.1086/629800
EISSN:: 1537-5269
ISSN:: 0022-1376

Item Description

Pubs id:: pubs:165099
UUID:: uuid:71df4c5c-c6fa-4d45-8d2d-297a2d4aa6e8
Local pid:: pubs:165099
Source identifiers:: 165099
Deposit date:: 2012-12-19

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Copyright date:: 1996

Licence:: Terms and Conditions of Use for Oxford University Research Archive

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