Fluid circulation in the South Tibetan Detachment System: Evidence from fluid inclusions and oxygen isotope data of quartz veins in the Ramba Dome, North Himalayan Gneiss Domes

2021 ◽  
Author(s):  
Xiaorong Li ◽  
Bo Zhang ◽  
Feng Cheng ◽  
Jinjiang Zhang ◽  
Yang Wang ◽  
...  
Keyword(s):  
Oxygen Isotope ◽  
Fluid Inclusions ◽  
Fluid Circulation ◽  
The South ◽  
Gneiss Domes ◽  
Quartz Veins ◽  
Isotope Data ◽  
Oxygen Isotope Data

scholarly journals Emerald from the Fazenda Bonfim Deposit, northeastern Brazil: chemical, fluid inclusions and oxygen isotope data

2018 ◽  
Vol 48 (3) ◽  
pp. 457-472 ◽  
Author(s):  
Judiron Santos Santiago ◽  
Valmir da Silva Souza ◽  
Bernardo de Carvalho Filgueiras ◽  
Federico Alberto Cuadros Jiménez
Keyword(s):  
Oxygen Isotope ◽  
Fluid Inclusions ◽  
Northeastern Brazil ◽  
Isotope Data ◽  
Oxygen Isotope Data

Tracing the emerald origin by oxygen isotope data: the case of Sandawana, Zimbabwe

2004 ◽  
Vol 336 (1) ◽  
pp. 41-48 ◽  
Author(s):  
Johannes C.(Hanco) Zwaan ◽  
Alain Cheilletz ◽  
Bruce E. Taylor
Keyword(s):  
Oxygen Isotope ◽  
Isotope Data ◽  
Oxygen Isotope Data

scholarly journals Oxygen isotope composition of zircons from the Talnakh economic intrusion of the Noril’sk province: first data

2019 ◽  
Vol 489 (2) ◽  
pp. 170-173
Author(s):  
I. Yu. Badanina ◽  
E. A. Belousova ◽  
K. N. Malitch ◽  
S. F. Sluzhenikin
Keyword(s):  
Oxygen Isotope ◽  
Isotope Composition ◽  
Oxygen Isotope Composition ◽  
Primary Magma ◽  
Crustal Component ◽  
Layered Series ◽  
Isotope Data ◽  
Oxygen Isotope Data ◽  
First Results ◽  
Isotope Analyses

This study presents the first results of oxygen isotope analyses (18O) collected on zircons from the Talnakh economic intrusion within the Norilsk province. Zircons from gabbro-diorite, gabbroic rocks of the layered series and plagioclase-bearing wehrlite have similar mantle-like mean 18O values (5,39 0,49; 5,64 0,48 and of 5,28 0,34, respectively), which differ from 18O in zircons from sulfide-bearing melanocratic troctolite with a taxitic texture in the lower part of the intrusion (mean 18O = 6,50 0,98). These new oxygen isotope data support (i) the mantle-derived origin of the primary magma(s), parental to the Talnakh intrusion, and (ii) possible involvement of a crustal component during the formation of sulfide-bearing taxitic-textured rocks.

scholarly journals New triple oxygen isotope data of bulk and separated fractions from SNC meteorites: Evidence for mantle homogeneity of Mars

2016 ◽  
Vol 51 (5) ◽  
pp. 981-995 ◽  
Author(s):  
Arshad Ali ◽  
Iffat Jabeen ◽  
David Gregory ◽  
Robert Verish ◽  
Neil R. Banerjee
Keyword(s):  
Oxygen Isotope ◽  
Isotope Data ◽  
Oxygen Isotope Data
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