Diamonds, Kimberlites, Lamproites and Related Rocks in the United States (Explor. Mining Geol., Vol. 4, No. 3, pp. 243-270, 1995)

Canadian Institute of Mining, Metallurgy and Petroleum
W. Dan Hausel
Organization:
Canadian Institute of Mining, Metallurgy and Petroleum
Pages:
28
File Size:
395 KB
Publication Date:
Jan 1, 1995

Abstract

"Hundreds of diamonds have been found in the United States. The majority of the discoveries occurred during the 19th century as a by-product of placer gold mining. Most of these early diamond finds have no known source, and in many cases are situated in areas unfavorable for diamond exploration based on current models that require kimberlite or lamproite to be emplaced in a stable Archean craton or Proterozoic craton margin.Diamonds have also been recovered in situ from lamproite at Murfreesburo, Arkansas, from kimberlite in the Lake Ellen region of Michigan, and in several kimberlites in the Colorado–Wyoming State Line district. Unverifed reports also suggest that diamonds may have been recovered from other related intrusions at a number of localities in the United States.IntroductionTo date, diamonds have been recovered in situ from kimberlite in the Colorado–Wyoming State Line district and from a kimberlite in Michigan. Additionally, diamonds have been recovered from lamproites in Arkansas. Diamonds have also been reported from kimberlite in Kansas, and from peridotite in New York and Maryland. However, these latter reports have not been verified."
Citation

APA: W. Dan Hausel  (1995)  Diamonds, Kimberlites, Lamproites and Related Rocks in the United States (Explor. Mining Geol., Vol. 4, No. 3, pp. 243-270, 1995)

MLA: W. Dan Hausel Diamonds, Kimberlites, Lamproites and Related Rocks in the United States (Explor. Mining Geol., Vol. 4, No. 3, pp. 243-270, 1995). Canadian Institute of Mining, Metallurgy and Petroleum, 1995.

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