scholarly journals Distribution and chemistry of kimberlite indicator minerals, Aylmer Lake map area (76C), Northwest Territories

1995 ◽  
Author(s):  
L A Dredge ◽  
I M Kjarsgaard ◽  
B C Ward ◽  
D E Kerr ◽  
J A R Stirling

2021 ◽  
Author(s):  
I R Smith ◽  
S J A Day ◽  
R C Paulen ◽  
D G Pearson

Till (n=196) and stream sediment (n=60) samples were collected in the area south and west of Great Slave Lake, Northwest Territories (NTS 85B, C, F, and G), over the course of 3 summer field seasons. Samples were processed to recover kimberlite and other indicator minerals. This report summarizes results of the kimberlite indicator mineral (KIM) studies, including measures of KIM mineral types, abundances, and chemistry (major, trace, and rare earth elements). KIMs were present in 24% of the samples collected, and only 183 KIM grains in total were recovered, of which Cr-pyrope garnets were the most abundant (65.6%). Chemical analyses revealed strong similarities to the Drybones Bay and Mud Lake kimberlites which are situated 50 to >100 km to the northeast, roughly aligned with prominent glacially streamlined landform flowsets in this field area. Results suggest there is little evidence for undetected kimberlite outcrop or sub-crop in the study area.





1995 ◽  
Author(s):  
B C Ward ◽  
I M Kjarsgaard ◽  
L A Dredge ◽  
D E Kerr ◽  
J A R Stirling


1995 ◽  
Author(s):  
D E Kerr ◽  
I M Kjarsgaard ◽  
B C Ward ◽  
L A Dredge ◽  
J A R Stirling


1997 ◽  
Author(s):  
L A Dredge ◽  
K E Kerr ◽  
I M Kjarsgaard ◽  
R D Knight ◽  
B C Ward


1996 ◽  
Author(s):  
D E Kerr ◽  
I M Kjarsgaard ◽  
L A Dredge ◽  
B C Ward ◽  
J A R Stirling


Author(s):  
J. B. Allen ◽  
T. Deans

SummaryA detrital assemblage of magnesian ilmenite, pyrope, chrome-diopside, rutile, and zircon has been traced to outcropping ultrabasic alkaline rocks, hitherto unknown in the Melanesian region. Analyses and descriptions of these ‘kimberlite indicator minerals’ are given. The host rocks comprise alnöite, an alnöite breccia with calcite matrix, and a magnesian ankaratrite, which are described, with chemical analyses. Emphasis is laid on the abundance of ultrabasic inclusions and xenocrysts and the replacements and transformations they have undergone. Malaita Island promises to contribute significantly to the understanding of the relations between alnöite, melilite basalts, and kimberlites.



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