Steven B. Shirey
Carnegie Institution for Science, Washington, DC
Activity
2024
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CONSTRAINTS ON DIAMOND DEPTHS OF ORIGIN FROM Fe-Mg PARTITIONING
T164 Gem Minerals, Localities and Geological SignificanceTuesday, 24 September 20248:00 AM - 12:00 PM207A
2022
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EVIDENCE FOR PRIMARY CARBONATE IN BERMUDA SI-UNDERSATURATED MAGMAS
27 D27. Recent Advances in Igneous Petrology and Volcanology (Posters)Sunday, 9 October 20229:00 AM - 1:00 PMExhibit Hall F
2021
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SUBDUCTION BEYOND THE ISLAND ARC AND MANTLE WEDGE: EVIDENCE FROM SUBLITHOSPHERIC DIAMONDS AND DEEP EARTHQUAKES
T62 Feedbacks between Upper-Plate Deformation, Accretion and Alteration and Plate Boundary Processes in Subduction Systems (Posters)Sunday, 10 October 20212:30 PM - 6:30 PMExhibit Hall A
2019
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NATURAL KIND CLUSTERING, PLANETARY EVOLUTION, AND THE CLASSIFICATION OF CARBON-BEARING MINERALS
234 D14. Recent Advances in Mineralogy/CrystallographyWednesday, 25 September 20198:00 AM - 12:00 PMRoom 125AB, North Building
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DIAMOND — PREMIER MINERAL FOR UNDERSTANDING THE DEEP GEOLOGY OF EARTH’S MANTLE
T137 Mineralogical Society of America (MSA) at 100: Reflections, Refractions, Diffractions, Intrusions, Subductions, Reactions, etc. from MSA Past Presidents IIMonday, 23 September 20191:30 PM - 5:30 PMRoom 131ABC, North Building
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THE TRANSITION FROM HADEAN CRUSTAL WORKING TO ARCHEAN CRATON GROWTH: THE EXAMPLE FROM THE SLAVE CRATON
T61 Life and Death of a Craton: Implications of Archean Crust-Keel Systems for Crustal Growth, Crustal Preservation, and Mantle EvolutionSunday, 22 September 20191:30 PM - 5:30 PMRoom 131ABC, North Building
2018
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S, PB, AND OS ISOTOPIC STUDIES OF MASSIVE NI-CU±PGE SULFIDES HOSTED IN METASEDIMENTARY COUNTRY ROCKS OF THE MIDCONTINENT RIFT SYSTEM, USA
T151 Geology and Fluid Dynamics of Cr, Ni-Cu-PGE, and PGE Mineralized Magmatic Plumbing SystemsTuesday, 6 November 20188:00 AM - 12:00 PMRoom 233
2017
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DIAMOND FORMATION THROUGH ISOCHEMICAL COOLING OF CHO FLUIDS VS REDOX BUFFERING: EXAMPLES FROM MARANGE PERIDOTITIC AND ZIMMI ECLOGITIC DIAMONDS
T172 Gemological Research in the 21st Century—Characterization, Exploration, and Geological Significance of Diamonds and other Gem Minerals (Posters)Monday, 23 October 20179:00 AM - 6:30 PMHalls 4EF
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TYPE IIB BORON-BEARING DIAMONDS ARE SUPERDEEP DIAMONDS
T20 Gemological Research in the 21st Century—Characterization, Exploration, and Geological Significance of Diamonds and other Gem MineralsSunday, 22 October 20178:00 AM - 12:00 PMSkagit 3
2016
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PRIMITIVE BASALTS OF THE POISON LAKE CHAIN: ISOTOPE RATIOS DISTINGUISH DIVERSE SOURCE COMPOSITIONS IN THE SOUTHERN CASCADES
256 Recent Advances in Igneous Petrology and Geochemistry (Posters)Tuesday, 27 September 20169:00 AM - 6:30 PMExhibit Hall E/F
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A SUBLITHOSPHERIC MANTLE, METALLIC LIQUID ORIGIN FOR THE WORLD'S LARGEST GEM-QUALITY DIAMONDS
T136 Gemological Research in the Twenty-First Century: Characterization, Exploration, and Geological Significance of Diamonds and Other Gem MineralsMonday, 26 September 20161:30 PM - 5:30 PMRoom 207
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UNUSUAL GEOLOGICAL HISTORY OF RARE TYPE IB DIAMONDS AND THE REASONS FOR THEIR SPECIAL COLOUR
T136 Gemological Research in the Twenty-First Century: Characterization, Exploration, and Geological Significance of Diamonds and Other Gem MineralsMonday, 26 September 20161:30 PM - 5:30 PMRoom 207
2015
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MSA PRESIDENTIAL ADDRESS: DIAMOND — PREMIER MINERAL FOR UNDERSTANDING THE GEOLOGY OF THE DEEP EARTH
258 Mineralogical Society of America (MSA) Awards Lectures, Presidential Address, and Annual Business MeetingTuesday, 3 November 20153:00 PM - 5:30 PMRoom 317
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NEOPROTEROZIC RE-OS AGE OF A SULFIDE INCLUSION IN A SUPERDEEP DIAMOND: IMPLICATIONS FOR MANTLE CONVECTION BENEATH JUINA, BRAZIL
T64 Gemological Research in the 21st Century: Exploration, Geology, and Characterization of Diamonds and other Gem MineralsSunday, 1 November 20151:30 PM - 5:30 PMRoom 342
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TYPE IB DIAMOND FORMATION RELATED TO GONDWANA ASSEMBLY: EVIDENCE FROM RE-OS ISOTOPIC COMPOSITIONS OF WEST AFRICAN SULPHIDE INCLUSIONS
T64 Gemological Research in the 21st Century: Exploration, Geology, and Characterization of Diamonds and other Gem MineralsSunday, 1 November 20151:30 PM - 5:30 PMRoom 342
2014
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GROWTH CONDITIONS OF MIXED-HABIT DIAMONDS FROM MARANGE, ZIMBABWE
T104 Gemological Research in the 21st Century: Exploration, Geology, and Characterization of Diamonds and Other Gem Minerals IMonday, 20 October 20148:00 AM - 12:00 PM202/203
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LOOKING AT OCEAN ISLANDS FROM THE BOTTOM: THE OSMIUM ISOTOPIC COMPOSITION OF SAVAI’I AND TUBUAI’I (SAMOA) MANTLE XENOLITHS
T14 Magmas and Their Sources I: A Tribute to the Distinguished Career of Fred FreySunday, 19 October 20148:00 AM - 12:00 PM205/206
2013
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RECENT ADVANCES IN THE UNDERSTANDING OF THE DISTRIBUTION, ORIGIN, AGE, AND GEOLOGICAL OCCURRENCES OF DIAMONDS
T218 Gemological Research in the 21st Century: Characterizing Diamonds and other Gem MineralsTuesday, 29 October 20138:00 AM - 12:00 PMRoom 205
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ISOTOPIC AND GEOPHYSICAL PERSPECTIVES ON DEEP MANTLE PROCESSES FOR CONSTRUCTING CRATONS
T124 Proterozoic Meets Archean: Amalgamation of LaurentiaMonday, 28 October 20138:00 AM - 12:00 PMRoom 304
2012
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DIAMONDS AND THE GEOLOGY OF EARTH MANTLE CARBON
211 Understanding Earth through CarbonWednesday, 7 November 20128:00 AM - 12:00 PMBallroom B
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SOURCES OF SULFUR AND CONTAMINATION IN CONDUIT TYPE MAGMATIC NI-SULFIDE DEPOSITS: EVIDENCE FROM THE MIDCONTINENT RIFT SYSTEM-ASSOCIATED TAMARACK INTRUSION, MINNESOTA
257 Economic GeologyWednesday, 7 November 20121:30 PM - 5:30 PM211AB
2011
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SCLM AND CRUSTAL EVIDENCE FOR 3 GA ONSET OF PLATE TECTONICS WITH IMPLICATIONS FOR THE SUPERIOR PROVINCE
T74 The Archean of North America: The Core of a ContinentMonday, 10 October 20118:00 AM - 12:00 PMRoom 200H-J
2008
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Re-Os Isotopic Study of the Eagle Ni-Cu Sulfide Deposit, Northern Michigan
256 Economic GeologyTuesday, 7 October 20081:30 PM - 5:30 PM
2006
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THE KAAPVAAL CRATON PROJECT: ORIGIN AND EVOLUTION OF CONTINENTAL LITHOSPHERE
T81 NSF Continental Dynamics Field Laboratories I: 20 Years OnMonday, 23 October 20068:00 AM - 12:00 PM