Skip to Main Content
Frequently Asked Questions
Submit an ETD
Global Search Box
Need Help?
Keyword Search
Participating Institutions
Advanced Search
School Logo
Files
File List
Schubel_1987_geology.pdf (38.96 MB)
ETD Abstract Container
Abstract Header
Petrographic Criteria for the Recognition of 'Magadi-Type' Cherts
Author Info
Schubel, Kathryn A
Permalink:
http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1415351823
Abstract Details
Year and Degree
1987, BA, Oberlin College, Geology.
Abstract
The Magadi cherts, inorganic lacustrine deposits from the Lake Magadi area, Kenya, are widely used as a modern analog to explain the origin of ancient inorganic cherts. Formed in a highly alkaline lake, as the result of a transformation from the sodium silicates minerals, magadiite and/or kenyaite, to quartz, the Magadi cherts possess a distinctive set of textural characteristics that allow them to be distinguished from cherts of different origin with only a limited number of samples. Textural characteristics that are diagnostic of the Magadi cherts and that can be used as a test for the occurrence of ancient 'Magadi-type' cherts are: 1) groundmass textures, which lie on a continuum from equigranular mosaics to grid-works, 2) variable concentrations of groundmass inclusions which occur as washes, clots, and fragments, 3) morphology, location, and orientation of cracks, fenestrae, and their filling phases, and 4) crystal molds. The transformation from magadiite to chert is accompanied by a 25% volume loss which is accommodated by the formation of shrinkage cracks, both internal and external, most similar in morphology and infill to subaqueously formed shrinkage cracks in clays and concretions, respectively. Textural and paragenetic criteria appear to be a valid test for the presence of 'Magaditype' cherts. Because important paleoenvironmental interpretations are made based on the presence of 'Magadi-type' cherts, it is important to have diagnostic tests to aid in its recognition. Further field work, and comparisons with lacustrine cherts of intermediate age are clearly needed at this point.
Committee
Bruce Simonson (Advisor)
Pages
65 p.
Subject Headings
Geology
Keywords
Magadi
;
cherts
;
Lake Magadi
;
Kenya
;
Magadi-type
;
Recommended Citations
Refworks
EndNote
RIS
Mendeley
Citations
Schubel, K. A. (1987).
Petrographic Criteria for the Recognition of 'Magadi-Type' Cherts
[Undergraduate thesis, Oberlin College]. OhioLINK Electronic Theses and Dissertations Center. http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1415351823
APA Style (7th edition)
Schubel, Kathryn.
Petrographic Criteria for the Recognition of 'Magadi-Type' Cherts.
1987. Oberlin College, Undergraduate thesis.
OhioLINK Electronic Theses and Dissertations Center
, http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1415351823.
MLA Style (8th edition)
Schubel, Kathryn. "Petrographic Criteria for the Recognition of 'Magadi-Type' Cherts." Undergraduate thesis, Oberlin College, 1987. http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1415351823
Chicago Manual of Style (17th edition)
Abstract Footer
Document number:
oberlin1415351823
Download Count:
158
Copyright Info
© 1987, all rights reserved.
This open access ETD is published by Oberlin College Honors Theses and OhioLINK.
Release 3.2.12