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Paul Kapp
Researcher at University of Arizona
Publications - 145
Citations - 16178
Paul Kapp is an academic researcher from University of Arizona. The author has contributed to research in topics: Terrane & Zircon. The author has an hindex of 55, co-authored 137 publications receiving 13312 citations. Previous affiliations of Paul Kapp include University of California, Los Angeles.
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Geological records of the Lhasa-Qiangtang and Indo-Asian collisions in the Nima area of central Tibet
TL;DR: A geological and geochronologic investigation of the Nima area along the Jurassic-Early Cretaceous Bangong suture of central Tibet provides well-dated records of contractional deformation and sedimentation during mid-Cretaceous and mid-Tertiary time as mentioned in this paper.
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Cretaceous-Tertiary shortening, basin development, and volcanism in central Tibet
TL;DR: The geologic map pattern of the Qiangtang terrane in central Tibet defines a >600km-long and up to 270km-wide east-plunging structural culmination as mentioned in this paper.
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Detrital zircon geochronology of pre-Tertiary strata in the Tibetan-Himalayan orogen
George E. Gehrels,Paul Kapp,Peter G. DeCelles,Alex Pullen,R. Blakey,Amy L. Weislogel,Lin Ding,Jerome H. Guynn,Aaron J. Martin,Nadine McQuarrie,An Yin +10 more
TL;DR: In this paper, the authors used 13,441 new or existing U-Pb ages of zircon crystals from strata in the Lesser Himalayan, Greater Himalayan and Tethyan sequences in the Himalaya, the Lhasa, Qiangtang, and Nan Shan-Qilian Shan-Altun Shan terranes in Tibet, and platformal strata of the Tarim craton to constrain changes in provenance through time.
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Paleocene–Eocene record of ophiolite obduction and initial India‐Asia collision, south central Tibet
Lin Ding,Paul Kapp,Xiaoqiao Wan +2 more
TL;DR: In this paper, the authors show that detrital chromium-rich spinels of ophiolite affinity (TiO2 generally < 0.1 wt%) were obtained from the Yarlung Zangbo suture in south central Tibet.
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Cyclicity in Cordilleran orogenic systems
TL;DR: In this article, an alternative model was proposed to explain key features of Cordilleran orogenic systems, such as cyclical trends in the flux and composition of magma supplied to the upper plate, and the foundering of arc roots.