Eben Blake Hodgin
Harvard University, Cambridge, MA
Activity
2020
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CRYOGENIAN RIFTING IN DEATH VALLEY, CALIFORNIA (USA)
T173 Assembling Laurentia: Neoproterozoic to Cambrian Rifting and Continental Margin Evolution during Breakup of Rodinia and PannotiaThursday, 29 October 202010:00 AM - 12:00 PMMeeting Rooms
2019
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TECTONIC SYNTHESIS OF THE TACONIC OROGENY FROM NEW ENGLAND TO NEWFOUNDLAND
T291 New Developments in the Appalachian-Caledonian-Variscan Orogen IIWednesday, 25 September 20191:30 PM - 5:30 PMRoom 229B, North Building
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RODINIA SUPERCONTINENT CONSTRAINTS FROM THE AREQUIPA TERRANE IN SOUTHERN PERU
T165 Structure and Tectonic Studies, from Outcrop to Supercontinent I: In Honor of Ian DalzielTuesday, 24 September 20198:00 AM - 12:00 PMRoom 229A, North Building
2018
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TESTING THE PRIMARY EXPRESSION OF THE SHURAM ISOTOPE EXCURSION ACROSS A BASIN TRANSECT OF THE SAN JUAN FORMATION, SOUTHERN PERU
T216 Evolving Perspectives of the Precambrian World: Using Combined Theoretical and Applied Approaches to Tackle Problems at the Intersection of Geology, Geobiology, and GeochemistryTuesday, 6 November 20181:30 PM - 5:30 PMRoom 242
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TONIAN AND CRYOGENIAN BASIN FORMATION IN DEATH VALLEY, CALIFORNIA AND THE PALEOENVIRONMENTAL CONTEXT OF THE PAHRUMP GROUP
T87 Earth and Life Co-Evolution in the Early to Middle Neoproterozoic (1000 to ca. 635 Ma)Monday, 5 November 20188:00 AM - 12:00 PMRoom 143-144
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REASSESSING THE MAIN IAPETAN SUTURE IN WESTERN NEWFOUNDLAND: NEW GEOCHRONOLOGICAL CONSTRAINTS ON THE TECTONIC HISTORY OF DASHWOODS AND CORNER BROOK
51 Orogenic Sutures—Recognition, Characterization, and Tectonic ImplicationsTuesday, 20 March 20188:00 AM - 12:00 PMDiamond Ballroom II
2017
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A PORPOISING CRYOGENIAN BASIN IN THE PANAMINT RANGE, CALIFORNIA
T344 New Perspectives on Cordilleran Tectonics, Paleogeography, and MetallogenyWednesday, 25 October 20171:30 PM - 5:30 PMTahoma 5
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DISPLACED CAMBRIAN BASINS AND CAMBRIAN STRIKE-SLIP EMPLACEMENT OF THE AREQUIPA TERRANE IN SOUTHERN PERU
T213 Understanding the Interplay of Structural, Metamorphic, and Magmatic Processes in the Evolution of Convergent Margins: Lessons from the Proterozoic to Present-Day South American Andean MarginTuesday, 24 October 20178:00 AM - 12:00 PMTahoma 2
2016
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CAMBRIAN STRIKE-SLIP EMPLACEMENT OF PAMPIA AND AREQUIPA ON CORDILLERAN MARGIN OF AMAZONIA: EVIDENCE FROM GEOCHRONOLOGY OF THE UMACHIRI FORMATION, PERU
T267 Plate Tectonics, Arc-Trench Systems, Cordilleran Tectonics, Sedimentary Basins, Sandstone Provenance, and Geoarchaeology (Posters): A Celebration of William R. Dickinson's CareerTuesday, 27 September 20169:00 AM - 6:30 PMExhibit Hall E/F
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GEOCHRONOLOGY OF THE GASKIERS GLACIATION
T259 Frontiers in Geochronology: Ancient Systems and Planetary Environments (Posters)Tuesday, 27 September 20169:00 AM - 6:30 PMExhibit Hall E/F
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WHY ARE CRYOGENIAN GLACIAL DEPOSITS ARE LOCALLY THICK, WHILE REGIONALLY THIN?: CASE STUDIES FROM THE OTAVI GROUP OF NAMIBIA
167 Precambrian Geology (Posters)Monday, 26 September 20169:00 AM - 6:30 PMExhibit Hall E/F
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TACONIC BASIN FORMATION AND MAGMATISM IN NEW ENGLAND AND NEWFOUNDLAND
30 Integrating Complementary Records of Paleozoic Orogenies in the Appalachians: Bridging the Foreland and HinterlandTuesday, 22 March 20168:00 AM - 12:00 PMMeeting Room 2
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WAS THE AREQUIPA MASSIF THE CONJUGATE RIFTED MARGIN OF NORTHEASTERN LAURENTIA?
1 A New Look at Terrane Affinity of Old Rocks in Western New England: Peri-Laurentian or Peri-Gondwana?Monday, 21 March 20168:00 AM - 10:00 AMMeeting Room 4
2015
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WAS THE AREQUIPA MASSIF THE CONJUGATE RIFTED MARGIN OF EASTERN LAURENTIA?
T341 Deconstructing Rodinia: Neoproterozoic-Cambrian Geologic Evolution of Laurentia’s MarginsWednesday, 4 November 20151:30 PM - 5:30 PMRoom 314