Related references
Note: Only part of the references are listed.The transition zone as a host for recycled volatiles: Evidence from nitrogen and carbon isotopes in ultra-deep diamonds from Monastery and Jagersfontein (South Africa)
M. Palot et al.
CHEMICAL GEOLOGY (2017)
Dated eclogitic diamond growth zones reveal variable recycling of crustal carbon through time
S. Timmerman et al.
EARTH AND PLANETARY SCIENCE LETTERS (2017)
Diamonds from Dachine, French Guiana: A unique record of early Proterozoic subduction
Chris B. Smith et al.
LITHOS (2016)
Carbon and nitrogen isotope systematics in diamond: Different sensitivities to isotopic fractionation or a decoupled origin?
K. Hogberg et al.
LITHOS (2016)
A nitrogen isotope fractionation factor between diamond and its parental fluid derived from detailed SIMS analysis of a gem diamond and theoretical calculations
D. C. Petts et al.
CHEMICAL GEOLOGY (2015)
Diamond Formation: A Stable Isotope Perspective
Pierre Cartigny et al.
ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 42 (2014)
Constraining the internal variability of the stable isotopes of carbon and nitrogen within mantle diamonds
S. Mikhail et al.
CHEMICAL GEOLOGY (2014)
Peridotitic and websteritic diamondites provide new information regarding mantle melting and metasomatism induced through the subduction of crustal volatiles
S. Mikhail et al.
GEOCHIMICA ET COSMOCHIMICA ACTA (2013)
Re-Os dating of sulphide inclusions zonally distributed in single Yakutian diamonds: Evidence for multiple episodes of Proterozoic formation and protracted timescales of diamond growth
D. F. Wiggers de Vries et al.
GEOCHIMICA ET COSMOCHIMICA ACTA (2013)
AVIAT DIAMONDS: A WINDOW INTO THE DEEP LITHOSPHERIC MANTLE BENEATH THE NORTHERN CHURCHILL PROVINCE, MELVILLE PENINSULA, CANADA
Jennifer Peats et al.
CANADIAN MINERALOGIST (2012)
Evidence for deep mantle convection and primordial heterogeneity from nitrogen and carbon stable isotopes in diamond
M. Palot et al.
EARTH AND PLANETARY SCIENCE LETTERS (2012)
The micro-/macro-diamond relationship: A case study from the Artemisia kimberlite (Northern Slave Craton, Canada)
C. N. Johnson et al.
LITHOS (2012)
Mixed fluid sources involved in diamond growth constrained by Sr-Nd-Pb-C-N isotopes and trace elements
Ofra Klein-BenDavid et al.
EARTH AND PLANETARY SCIENCE LETTERS (2010)
Biological activity and the Earth's surface evolution: Insights from carbon, sulfur, nitrogen and iron stable isotopes in the rock record
Christophe Thomazo et al.
COMPTES RENDUS PALEVOL (2009)
Metasomatic diamond growth: A multi-isotope study (13C, 15N, 33S, 34S) of sulphide inclusions and their host diamonds from Jwaneng (Botswana)
E. Thomassot et al.
EARTH AND PLANETARY SCIENCE LETTERS (2009)
Diamond origin and genesis: A C and N stable isotope study on diamonds from a single eclogitic xenolith (Kaalvallei, South Africa)
Mederic Palot et al.
LITHOS (2009)
A mantle origin for Paleoarchean peridotitic diamonds from the Panda kimberlite, Slave Craton: Evidence from 13C-, 15N- and 33,34S-stable isotope systematics
Pierre Cartigny et al.
LITHOS (2009)
Stable isotopes and the origin of diamond
P Cartigny
ELEMENTS (2005)
Mineral inclusions in microdiamonds and macrodiamonds from kimberlites of Yakutia: a comparative study
NV Sobolev et al.
LITHOS (2004)
Constraining diamond metasomatic growth using C- and N-stable isotopes: examples from Namibia
P Cartigny et al.
LITHOS (2004)
Diamond genesis, mantle fractionations and mantle nitrogen content:: a study of δ13C-N concentrations in diamonds
P Cartigny et al.
EARTH AND PLANETARY SCIENCE LETTERS (2001)
Share Paper
