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
kent1240007954.pdf (29.74 MB)
ETD Abstract Container
Abstract Header
Reconnaissance U-Pb geochronology of Precambrian crystalline rocks from the northern Black Hills, South Dakota: Implications for regional thermotectonic history
Author Info
Ghosh, Amiya Kumar
Permalink:
http://rave.ohiolink.edu/etdc/view?acc_num=kent1240007954
Abstract Details
Year and Degree
2009, MS, Kent State University, College of Arts and Sciences / Department of Earth Sciences.
Abstract
Th/U-bearing accessory minerals monazite, zircon, and titanite occurring in selected metamorphic and igneous rocks from the northern Black Hills (NBH), South Dakota, were analyzed by standard U-Pb radiometric methods to unravel the Precambrian thermotectonic events that affected the area. Four metapelites from the Crook Mountain borehole contain metamorphic monazites for which EMP spot-analysis yielded total-Pb dates ranging from ~2680-1600 Ma but mostly between ~1790-1650 Ma. Individual spot-dates obtained for the metapelites were grouped according to compositional domains, as revealed by X-ray imagery, whereupon the resultant domain ages resolved into four discrete age clusters of ~1780 ± 3 Ma (32% of the dates), ~1751 ± 3 Ma (44%), ~1718 ± 14 Ma (7%), and ~1650 ± 9 Ma (16%, all dates reported at 95% confidence). These dates correspond to thermotectonic and magmatic events previously recognized at these times in the southern Black Hills, and the timing of Homestake gold mineralization is constrained between ~1740 -1718 Ma. Spot-analysis of zircon grains extracted from a Crook Mountain granite pegmatite yielded 207Pb/206Pb upper- and lower-intercept ages of 1718 ± 22 Ma and 51 ± 17 Ma, which are interpreted as intrusive and uplift ages, respectively. Detrital zircons of magmatic origin from two Black Hills metapelites have also been spot-dated. Five 207Pb/206Pb age populations are recognized at: ~3830 ± 8, ~3365 ± 5, ~3425 ± 7, ~3240 ± 4, and ~2970 ± 11 Ma. These ages indicate zircon provenance from the ~3550-2550 Ma Wyoming craton rather than from the ~2900-2600 Ma Superior craton. Thus, the Black Hills appears to have been part of the Wyoming craton as of 2015-1880 Ma shale deposition.
Committee
Peter Dahl, PhD (Advisor)
Abdul Shakoor, PhD (Committee Member)
Daniel Holm, PhD (Committee Member)
Pages
131 p.
Subject Headings
Geochemistry
;
Geology
Keywords
Black Hills
;
Crook Mountain granite
;
Homestake gold mine
;
gold mineralization
;
magmatism
;
metamorphism
;
metapelite
;
g monazite
;
zircon
;
titanite
;
geochronology
;
thermotectonism
Recommended Citations
Refworks
EndNote
RIS
Mendeley
Citations
Ghosh, A. K. (2009).
Reconnaissance U-Pb geochronology of Precambrian crystalline rocks from the northern Black Hills, South Dakota: Implications for regional thermotectonic history
[Master's thesis, Kent State University]. OhioLINK Electronic Theses and Dissertations Center. http://rave.ohiolink.edu/etdc/view?acc_num=kent1240007954
APA Style (7th edition)
Ghosh, Amiya.
Reconnaissance U-Pb geochronology of Precambrian crystalline rocks from the northern Black Hills, South Dakota: Implications for regional thermotectonic history.
2009. Kent State University, Master's thesis.
OhioLINK Electronic Theses and Dissertations Center
, http://rave.ohiolink.edu/etdc/view?acc_num=kent1240007954.
MLA Style (8th edition)
Ghosh, Amiya. "Reconnaissance U-Pb geochronology of Precambrian crystalline rocks from the northern Black Hills, South Dakota: Implications for regional thermotectonic history." Master's thesis, Kent State University, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=kent1240007954
Chicago Manual of Style (17th edition)
Abstract Footer
Document number:
kent1240007954
Download Count:
691
Copyright Info
© 2009, all rights reserved.
This open access ETD is published by Kent State University and OhioLINK.