Steven B. Shirey

Carnegie Institution for Science

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

Richard W. Carlson

Carnegie Institution for Science

D. Graham Pearson

University of Alberta

Stephen H. Richardson

Brigham Young University

Karen V. Smit

University of the Witwatersrand

Thomas Stachel

University of Alberta

Michael J. Walter

Carnegie Institution for Science

Jeffrey W. Harris

University of Glasgow

Richard A. Stern

University of Alberta

Fabrizio Nestola

University of Padua

Jeff W. Harris

Geoscience BC

Cooperative Institutions

Carnegie Institution for Science

University of Alberta

Carnegie Observatories

United States Geological Survey

University of Cape Town

Centre National de la Recherche Scientifique

Planetary Science Institute

Geophysical Laboratory

University of Bristol

University of Wisconsin–Madison

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

Archean subduction recorded by Re–Os isotopes in eclogitic sulfide inclusions in Kimberley diamonds

Earth and Planetary Science Letters (2001)

Stephen H. Richardson Steven B. Shirey Jeff W. Harris Richard W. Carlson

Radiogenic nuclide

Fractional crystallization (geology)

Protolith

10.1016/s0012-821x(01)00419-8

Cite

Citations (193)

Roberts Victor Eclogites: The MacGregor Legacy of Archean Oceanic Lithosphere Subduction and its Role in Craton Formation

AGU Fall Meeting Abstracts (2005)

Steven B. Shirey Mark D. Schmitz Uwe Wiechert Richard W. Carlson

Source

Cite

Citations (0)

Diamond formation episodes at the southern margin of the Kaapvaal Craton: Re–Os systematics of sulfide inclusions from the Jagersfontein Mine

Contributions to Mineralogy and Petrology (2008)

Sonja Aulbach Steven B. Shirey Thomas Stachel Steven Creighton Karlis Muehlenbachs

Peridotite

Radiogenic nuclide

Primitive mantle

Xenolith

Metasomatism

10.1007/s00410-008-0350-9

Cite

Citations (46)

Discriminating assimilants and decoupling deep- vs. shallow-level crystal records at Mount Adams using 238U–230Th disequilibria and Os isotopes

Earth and Planetary Science Letters (2008)

Brian R. Jicha Clark M. Johnson Wes Hildreth Brian L. Beard Garret L. Hart

Phenocryst

10.1016/j.epsl.2008.09.035

Cite

Citations (28)

The Lake Superior region and Trans-Hudson orogen

Geological Society of America eBooks (1993)

J. Lawford Anderson Robert L. Bauer V.W. Chandler Gilbert N. Hanson J. Kalliokoski

Abstract Precambrian rocks in the Lake Superior region underlie all or parts of Minnesota, Wisconsin, and Michigan, an area along the southern margin of the Superior province of the Canadian Shield (Fig. 1). Except on the north, adjacent to Canada, the Precambrian rocks are overlapped by sedimentary strata of Paleozoic and Mesozoic age, which constitute a thin platform cover of relatively undisturbed rocks that thicken to the west, south, and east. Inliers of Precambrian rocks are exposed locally in southern Minnesota and Wisconsin, mainly in the flat valleys of major rivers, where erosion has cut below the Phanerozoic strata. The present landscape is subdued, and is inherited largely from Pleistocene continental glaciations, which produced a variety of erosional and depositional landforms. The glacier ice scoured the bedrock in the northern parts of the region, in much the same way as throughout most of Canada, and deposited materials of diverse lithology and provenance, as much as 200 m thick, over much of the remainder of the region. The Precambrian rocks in the region record an extended interval of crustal development and evolution that spans nearly 3 b.y. of earth history. This interval of geologic time is not continuously recorded in layered and intrusive units, but instead is punctuated by specific rock-forming and tectonic events that can be deduced from geologic relations and placed in a chronometric framework by isotopic dating. (Fig. 2, also see correlation chart for Precambrian rocks of the Lake Superior region, Morey and Van Schmus, 1986; and Bergstrom and Morey, 1985.)

Laurentia

10.1130/dnag-gna-c2.11

Cite

Citations (22)

Mantle heterogeneity and crustal recycling in Archean granite-greenstone belts: Evidence from Nd isotopes and trace elements in the Rainy Lake area, Superior Province, Ontario, Canada

Geochimica et Cosmochimica Acta (1986)

Steven B. Shirey Gilbert N. Hanson

Greenstone belt

Trace element

Crustal recycling

Incompatible element

10.1016/0016-7037(86)90215-2

Cite

Citations (259)

Neoproterozoic Zimmi diamond formation through infiltration of recycled methane into sulphide-bearing Archaean eclogite

International Kimberlite Conference Extended Abstracts: 2008 (2019)

Karen V. Smit Steven B. Shirey E. H. Hauri Jianhua Wang Thomas Stachel

Infiltration (HVAC)

10.29173/ikc3924

Cite

Citations (0)

Genesis mechanisms and the survival and destruction of continental lithospheric mantle

Geochimica et Cosmochimica Acta (2006)

Richard W. Carlson Steven B. Shirey

10.1016/j.gca.2006.06.081

Cite

Citations (0)

Os, Sr, Nd, and Pb isotope systematics of southern African peridotite xenoliths: Implications for the chemical evolution of subcontinental mantle

Geochimica et Cosmochimica Acta (1989)

R. J. Walker Richard W. Carlson Steven B. Shirey Boyd F.R

Peridotite

Xenolith

Primitive mantle

10.1016/0016-7037(89)90240-8

Cite

Citations (694)

Diamonds and the Geology of Mantle Carbon

Reviews in Mineralogy and Geochemistry (2013)

Steven B. Shirey Pierre Cartigny D. J. Frost Satish Keshav Fabrizio Nestola

Research Article| January 01, 2013 Diamonds and the Geology of Mantle Carbon Steven B. Shirey; Steven B. Shirey Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road, NW, Washington, DC 20015, U.S.A., shirey@dtm.ciw.edu Search for other works by this author on: GSW Google Scholar Pierre Cartigny; Pierre Cartigny Laboratoire de Géochimie des Isotopes Stables de l’Institut de Physique du Globe de Paris, UMR 7154, Université Paris Denis-Diderot, PRES Sorbonne Paris-Cité, Office n°511, 1 rue Jussieu,75005 Paris, France Search for other works by this author on: GSW Google Scholar Daniel J. Frost; Daniel J. Frost Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany Search for other works by this author on: GSW Google Scholar Shantanu Keshav; Shantanu Keshav Geosciences Montpellier, University of Montpellier 2, CNRS & UMR 5243, Montpellier, France Search for other works by this author on: GSW Google Scholar Fabrizio Nestola; Fabrizio Nestola Department of Geosciences, University of Padua, Via Gradenigo 6, 1-35131 Padova, Italy Search for other works by this author on: GSW Google Scholar Paolo Nimis; Paolo Nimis Department of Geosciences, University of Padua, Via Gradenigo 6, 1-35131 Padova, Italy Search for other works by this author on: GSW Google Scholar D. Graham Pearson; D. Graham Pearson Department of Earth and Atmospheric Sciences, University of Alberta, 1-26 Earth Sciences Building, Edmonton, Alberta, Canada T6G 2E3 Search for other works by this author on: GSW Google Scholar Nikolai V. Sobolev; Nikolai V. Sobolev V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences, 630090 Novosibirsk 90, Russia Search for other works by this author on: GSW Google Scholar Michael J. Walter Michael J. Walter School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, United Kingdom Search for other works by this author on: GSW Google Scholar Author and Article Information Steven B. Shirey Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road, NW, Washington, DC 20015, U.S.A., shirey@dtm.ciw.edu Pierre Cartigny Laboratoire de Géochimie des Isotopes Stables de l’Institut de Physique du Globe de Paris, UMR 7154, Université Paris Denis-Diderot, PRES Sorbonne Paris-Cité, Office n°511, 1 rue Jussieu,75005 Paris, France Daniel J. Frost Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany Shantanu Keshav Geosciences Montpellier, University of Montpellier 2, CNRS & UMR 5243, Montpellier, France Fabrizio Nestola Department of Geosciences, University of Padua, Via Gradenigo 6, 1-35131 Padova, Italy Paolo Nimis Department of Geosciences, University of Padua, Via Gradenigo 6, 1-35131 Padova, Italy D. Graham Pearson Department of Earth and Atmospheric Sciences, University of Alberta, 1-26 Earth Sciences Building, Edmonton, Alberta, Canada T6G 2E3 Nikolai V. Sobolev V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences, 630090 Novosibirsk 90, Russia Michael J. Walter School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, United Kingdom Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © 2013 Mineralogical Society of America Reviews in Mineralogy and Geochemistry (2013) 75 (1): 355–421. https://doi.org/10.2138/rmg.2013.75.12 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Steven B. Shirey, Pierre Cartigny, Daniel J. Frost, Shantanu Keshav, Fabrizio Nestola, Paolo Nimis, D. Graham Pearson, Nikolai V. Sobolev, Michael J. Walter; Diamonds and the Geology of Mantle Carbon. Reviews in Mineralogy and Geochemistry 2013;; 75 (1): 355–421. doi: https://doi.org/10.2138/rmg.2013.75.12 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Earth’s carbon, derived from planetesimals in the 1 AU region during accretion of the Solar System, still retains similarities to carbon found in meteorites (Marty et al. 2013) even after 4.57 billion years of geological processing. The range in isotopic composition of carbon on Earth versus meteorites is nearly identical and, for both, diamond is a common, if volumetrically minor, carbon mineral (Haggerty 1999). Diamond is one of the three native carbon minerals on Earth (the other two being graphite and lonsdaleite). It can crystallize throughout the mantle below about 150 km and can occur metastably... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Globe

10.2138/rmg.2013.75.12

Cite

Citations (406)