Lin Ding
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing
Activity
2024
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ACCELERATING SUBSIDENCE, ANOMALOUS INTRABASINAL DEFORMATION, AND RAPID POST-BURIAL EXHUMATION IN AN ENIGMATIC EOCENE LACUSTRINE BASIN IN CENTRAL TIBET
T70 Innovative Ideas in Tectonics of Earth and Other Planetary Bodies II: a Session in Memory of An YinSunday, 22 September 20241:30 PM - 5:30 PM304C
2021
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TRENCH VERSUS FOREARC: LATE CRETACEOUS TRENCH SEDIMENT ACCUMULATION AND FOREARC EROSION ALONG THE SOUTHERN MARGIN OF TIBET AS REVEALED BY PROVENANCE ANALYSIS
T162 Initiation and Evolution of Arc-Forearc Systems in Cascadia and Beyond (Posters)Tuesday, 12 October 20219:00 AM - 1:00 PMExhibit Hall A
2020
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PUNCTUATED OROGENY DURING THE ASSEMBLY OF ASIA: PROTEROZOIC-PALEOZOIC GEOLOGIC HISTORY OF THE NORTH CHINA CRATON AND TIBETAN PLATEAU
T7 Topographic and Lithospheric Evolution of Elevated Continental Passive MarginsMonday, 26 October 20201:30 PM - 5:30 PMMeeting Rooms
2019
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WERE CENOZOIC BASINS, SHORTENING, AND MAGMATISM IN CENTRAL TIBET CAUSED BY LITHOSPHERIC DRIPPING?
T244 Integrated Tectono-Sedimentary Records in the Tibetan Plateau and Adjacent AreasWednesday, 25 September 20198:00 AM - 12:00 PMRoom 231ABC, North Building
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DETRITAL ZIRCON PROVENANCE ANALYSIS OF RONGMAWA FORMATION STRATA ALONG THE INDIA-ASIA SUTURE IN SOUTHERN TIBET SUGGEST THAT THE LHASA RIVER IS AN ANTECEDENT TRANS-ARC RIVER THAT TRANSPORTED SEDIMENT FROM THE CENTRAL LHASA TERRANE TO THE SUBDUCTION ZONE IN LATE CRETACEOUS TIME
T292 From Oceanic Subduction to Inter-Continental Collision: Examples of Convergent Margin Processes in Non-Collisional and Collisional SettingsWednesday, 25 September 20191:30 PM - 5:30 PMRoom 231ABC, North Building
2018
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DISCOVERY OF TWO NEW SEDIMENTARY SUCCESSIONS ALONG THE INDIA-ASIA COLLISION ZONE, TIBET
T287 The Cenozoic Evolution of Tibet—How Do We Unify Seemingly Contradictory Evidence?Wednesday, 7 November 20181:30 PM - 5:30 PMRoom 243
2017
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ACCRETION OF NEO-TETHYS OCEANIC SUBDUCTION IN EARLIEST CRETACEOUS ALONG THE YARLUNG ZANGBO SUTURE ZONE, SANGSANG AREA, SOUTHERN TIBET
T322 Polygenetic Mélanges: A Glimpse on Tectono-Sedimentary Recycling in Convergent MarginsWednesday, 25 October 20178:00 AM - 12:00 PMTahoma 5
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AN EARLY BIRD FROM GONDWANA: PALEOMAGNETISM OF LOWER PERMIAN LAVAS FROM NORTHERN QIANGTANG (TIBET) AND THE GEOGRAPHY OF THE PALEO-TETHYS
T218 Contributions of Rock- and Paleo-magnetism to Understanding Orogenic ProcessesTuesday, 24 October 20178:00 AM - 12:00 PMYakima 1
2015
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LHASA’S JURASSIC-TO-PALEOCENE LATITUDE: IMPLICATIONS FOR THE CENOZOIC TECTONICS AND CLIMATE OF TIBET
T7 Bridging Two Continents: Geologic Configuration of the Tibetan Plateau Region Prior to the Indo-Asian Collision: Setting the Stage for Development of a High Elevation PlateauSunday, 1 November 20158:00 AM - 12:00 PMRoom 347/348