T
Tinghong Zhou
Researcher at University of Rochester
Publications - 9
Citations - 279
Tinghong Zhou is an academic researcher from University of Rochester. The author has contributed to research in topics: Geology & Paleomagnetism. The author has an hindex of 2, co-authored 4 publications receiving 128 citations. Previous affiliations of Tinghong Zhou include Peking University.
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Paleomagnetic constraints on the paleogeography of the East Asian blocks during Late Paleozoic and Early Mesozoic times
TL;DR: In this article, a series of paleogeographic reconstructions for these major blocks and lesser terranes of East Asia between mid-Ordovician and late Jurassic times was presented.
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Permian Paleogeography of the Eastern CAOB: Paleomagnetic Constraints From Volcanic Rocks in Central Eastern Inner Mongolia, NE China
Donghai Zhang,Donghai Zhang,Baochun Huang,Jie Zhao,Joseph G. Meert,Ye Zhang,Yalun Liang,Qianhui Bai,Tinghong Zhou +8 more
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Quantifying the extent of the Paleo-Asian Ocean during the Late Carboniferous to Early Permian
Donghai Zhang,Donghai Zhang,Baochun Huang,Guochun Zhao,Guochun Zhao,Joseph G. Meert,Simon Williams,Simon Williams,Jie Zhao,Tinghong Zhou +9 more
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Absence of a long-lived lunar paleomagnetosphere.
John A. Tarduno,Rory D. Cottrell,Kristin Lawrence,Richard K. Bono,Wentao Huang,Catherine L. Johnson,Catherine L. Johnson,Eric G. Blackman,Aleksey V. Smirnov,Miki Nakajima,Clive R. Neal,Tinghong Zhou,Mauricio Ibanez-Mejia,Hirokuni Oda,Ben Crummins +14 more
TL;DR: In this article, it was shown that Apollo impact glass associated with a young 2 million-year-old crater records a strong Earth-like magnetization, providing evidence that impacts can impart intense signals to samples recovered from the Moon and other planetary bodies.
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Early Cambrian renewal of the geodynamo and the origin of inner core structure
Tinghong Zhou,John A. Tarduno,Francis Nimmo,Rory D. Cottrell,Richard K. Bono,Mauricio Ibanez-Mejia,Wentao Huang,Matthew W. Hamilton,Kenneth P. Kodama,Aleksey V. Smirnov,Ben Crummins,Frank Padgett +11 more
TL;DR: In this article , the seismic anisotropy of the outermost inner core reflects development of a global spherical harmonic degree-2 deep mantle structure at this time that has persisted to the present day.