Carbon isotopic composition, nitrogen content and inclusion composition of diamonds from the Roberts Victor kimberlite, South Africa: Evidence for 13C depletion in the mantle

1987 ◽  
Vol 51 (5) ◽  
pp. 1227-1243 ◽  
Author(s):  
Peter Deines ◽  
J.W Harris ◽  
J.J Gurney
1992 ◽  
Vol 37 (2) ◽  
pp. 203-213 ◽  
Author(s):  
A.S. Talma ◽  
John C. Vogel

AbstractAn oxygen isotope temperature record over a large part of the past 30,000 yr has been obtained for the southern Cape Province of South Africa by combining data on the isotopic composition of a stalagmite from a deep cave with that of a confined groundwater aquifer in the same region. Results show that temperatures during the last glacial maximum were on average about 6°C lower than those today, with peaks up to 7°C lower. A detailed analysis of the past 5000 yr suggests multiple fluctuations, with generally lower temperatures (1–2°C) around 4500 and 3000 yr B.P. The carbon isotopic composition of the stalagmite indicates significant vegetation changes between the late Pleistocene and today, and also during the second half of the Holocene.


2021 ◽  
Vol 43 (2) ◽  
pp. 3-11
Author(s):  
V.M. KVASNYTSYA

We studied a collection of microdiamonds from the Zeleny Yar Neogene placer on the Ros’-Tikych megablock of the Ukrainian Shield, which consists of 102 microdiamonds, with crystal sizes 0.2-0.5 mm, using crystal morphology, photoluminescence, infrared and Raman spectroscopy, isotopic composition of carbon and helium of microdiamonds. Crystal forms are dominantly octahedra, others are cubes, combinational crystals {111}+{110}+{100}, cube-octahedra, and transitional forms {111}+{110}; rhombic dodecahedrons are rare. Many microdiamonds are damaged crystals and their fragments. Up to 20% of the studied microdiamonds are yellow, green, pink-purple, brown, gray, and black. The most colored crystals are among the cubes. Up to 70% of the studied microdiamonds are blue, green, yellow and orange in ultraviolet light. Many of the microdiamonds, especially cubes and crystals of the combinational form {111}+{110}+{100}, have an orange photoluminescence (center at 575 nm). 50% of the crystals are nitrogen-free crystals of type IIa. Nitrogen crystals of type Ia amount to 45% (among them 29 % of subtype IaA, 11% of subtype IaAB and 5% of subtype Iab) and 5% of type Ib. The content of nitrogen ranges from 57 to 612 at. ppm with an average nitrogen content of 224 at. ppm. The centers B2 (lines 1358-1380 cm–1) and hydrogen centers (3107 cm–1, 1405 cm–1) were recorded in IR spectra of some microdiamonds. The Raman line ranges from 1331.25 cm–1 to 1331.75 cm–1 with FWHM from 2.04 cm–1 to 4.47 cm–1. The carbon isotopic composition of microdiamonds shows a very wide range from –26.74 to –3.55‰ δ13C PDB. The content of helium isotopes for the studied crystal is 73.42 × 10–12 cm3/g of 3He and 0.265 × 10–6 cm3/g of 4He. Given the wide range of values of the isotopic composition of carbon δ13C, relatively high nitrogen content and cubic form of many crystals, it is possible to predict the eclogite association as the mantle crystallization medium of the Zeleny Yar microdiamonds. The location of the parent rocks of the microdiamonds is assumed to be the Berdychiv uplift of the Podolia block of the Ukrainian Shield.


2021 ◽  
Vol 64 (3) ◽  
pp. 470-493 ◽  
Author(s):  
Jianping Chen ◽  
Xulong Wang ◽  
Jianfa Chen ◽  
Yunyan Ni ◽  
Baoli Xiang ◽  
...  

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