Mark Edward Holland
University of New Mexico, Albuquerque, NM
Activity
2016
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GROWTH AND EVOLUTION OF SOUTHERN LAURENTIA IN THE CONTEXT OF THE NUNA SUPERCONTINENT: PALEOPROTEROZOIC CONNECTIONS BETWEEN AUSTRALIA/ANTARCTICA (MAWSON) AND LAURENTIA
T230 Proterozoic Accretion of the North American Continent – United Plates of America Revisited IITuesday, 27 September 20161:30 PM - 5:30 PMMile High Ballroom 3B
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PROTEROZOIC ACCRETIONARY OROGENS OF SOUTHERN LAURENTIA REVISITED
T230 Proterozoic Accretion of the North American Continent – United Plates of America Revisited IITuesday, 27 September 20161:30 PM - 5:30 PMMile High Ballroom 3B
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PAIRED ZIRCON U-PB-HF ISOTOPE ANALYSIS OF THE YAVAPAI-MAZATZAL BOUNDARY IN NEW MEXICO: EVIDENCE FOR A MAZATZAL CONTINENTAL ARC SYSTEM
T139 Fifty Years of Innovation in Petrology and Orogenic Systems II: A Tribute to Lincoln HollisterMonday, 26 September 20161:30 PM - 5:30 PMRoom 205
2015
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GROWTH OF CONTINENTAL LITHOSPHERE BY ACCRETION OF ARC TERRANES ALONG THE LAURENTIAN MARGIN THROUGHOUT THE PROTEROZOIC: EVIDENCE FROM HF ISOTOPES
T287 Integrating Perspectives on the Formation, Evolution, and Destruction of Continental Crust: From 0 to 4600 MaWednesday, 4 November 20158:00 AM - 12:00 PMRoom 308
2013
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USING PAIRED U-PB AND HF ISOTOPES TO CHARACTERIZE THE CRUSTAL EVOLUTION OF THE MOJAVE PROVINCE: COMPARISON OF IGNEOUS AND METASEDIMENTARY LITHOLOGIES IN GRAND CANYON AND DEATH VALLEY
T124 Proterozoic Meets Archean: Amalgamation of LaurentiaMonday, 28 October 20138:00 AM - 12:00 PMRoom 304
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DETRITAL ZIRCON CHARACTERISTICS OF UNCONFORMITY-BOUND PROTEROZOIC METASEDIMENTARY SUCCESSIONS IN CENTRAL ARIZONA: RELATIVELY SHORT-LIVED SYNTECTONIC BASINS AS KEY ELEMENTS IN THE PROTEROZOIC TECTONIC EVOLUTION OF SOUTHWESTERN LAURENTIA
T189 Regional to Global Perspectives on the Formation, Assembly, and Tectonic Evolution of Western North America from the Neoarchean through the MesoproterozoicMonday, 28 October 20131:00 PM - 5:00 PMRoom 304
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THE PALEOPROTEROZOIC EVOLUTION OF THE ATHABASCA GRANULITE TERRANE (SNOWBIRD TECTONIC ZONE), WESTERN CHURCHILL PROVINCE, CANADA: DEFORMATION DUE TO FAR-FIELD OROGENIC PROCESSES
T124 Proterozoic Meets Archean: Amalgamation of LaurentiaMonday, 28 October 20138:00 AM - 12:00 PMRoom 304
2012
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DECIPHERING THE AGE AND SIGNIFICANCE OF LOWER CRUSTAL HIGH STRAIN ZONES: A CASE STUDY FROM THE CORA LAKE SHEAR ZONE, ATHABASCA GRANULITE TERRANE, SASKATCHEWAN
T133 Deformation Processes in Lithospheric High-Strain Zones IIMonday, 5 November 20121:30 PM - 5:30 PM208A
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THE MARY REACTION: TIMING DEEP CRUSTAL DEFORMATION AND METAMORPHISM WITH IMPLICATIONS FOR STRENGTHENING AND STABILIZATION OF FLOWING LOWER CRUST
51 Tectonics (Posters)Tuesday, 20 March 20128:00 AM - 12:00 PMBallrooms A, B & C and Ballroom Pre-function Area
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INTERPRETING THE TECTONIC HISTORY OF CRUSTAL-SCALE HIGH STRAIN ZONES: INSIGHTS FROM THE CORA LAKE SHEAR ZONE, WESTERN CHURCHILL PROVINCE
46 High-Strain Zone Kinematics, From the Microscopic to the Macroscopic ScaleTuesday, 20 March 20128:00 AM - 12:00 PMBallroom D