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Decoding Provenance and Tectonothermal Events by Detrital Zircon Fission-Track and U/Pb Double Dating: A Case of the Southern Ordos Basin

Published on Mar 12, 2019in Acta Geologica Sinica-english Edition 2.51
· DOI :10.1111/1755-6724.13802
Shaohua Zhang1
Estimated H-index: 1
(Northwest University (United States)),
Chiyang Liu5
Estimated H-index: 5
(Northwest University (United States))
+ 3 AuthorsHexin Huang7
Estimated H-index: 7
(Northwest University (United States))
  • References (88)
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References88
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Published on Dec 20, 2017in Geology 5.07
Michael S. DeLucia1
Estimated H-index: 1
(University of Illinois at Urbana–Champaign),
William R. Guenthner8
Estimated H-index: 8
(University of Illinois at Urbana–Champaign)
+ 2 AuthorsAlexis K. Ault9
Estimated H-index: 9
(Utah State University)
6 Citations Source Cite
Published on Oct 1, 2017in Acta Geologica Sinica-english Edition 2.51
Xiaochen Zhao1
Estimated H-index: 1
(Xi'an University of Science and Technology),
Chiyang Liu5
Estimated H-index: 5
(Northwest University (United States))
+ 4 AuthorsWei Luo2
Estimated H-index: 2
(Northwest University (United States))
2 Citations Source Cite
Published on Oct 1, 2017in Earth and Planetary Science Letters 4.58
Jie Xu4
Estimated H-index: 4
(China University of Geosciences),
Daniel F. Stockli49
Estimated H-index: 49
(University of Texas at Austin),
John W. Snedden8
Estimated H-index: 8
(University of Texas at Austin)
Abstract Detrital zircon U–Pb analysis is an effective approach for investigating sediment provenance by relating crystallization age to potential crystalline source terranes. Studies of large passive margin basins, such as the Gulf of Mexico Basin, that have received sediment from multiple terranes with non-unique crystallization ages or sedimentary strata, benefit from additional constraints to better elucidate provenance interpretation. In this study, U–Pb and (U–Th)/He double dating analyses...
4 Citations Source Cite
Published on Oct 1, 2017in Acta Geologica Sinica-english Edition 2.51
Beihang Zhang5
Estimated H-index: 5
,
Jin Zhang4
Estimated H-index: 4
+ 2 AuthorsYanfeng Li1
Estimated H-index: 1
The apatite fission track (AFT) ages and thermal modeling of the Longshoushan and deformation along the northern Hexi Corridor on the northern side of the Qinghai-Tibetan Plateau show that the Longshoushan along the northern corridor had experienced important multi-stage exhumations during the Late Mesozoic and Cenozoic. The AFT ages of 7 samples range from 31.9 Ma to 111.8 Ma. Thermal modeling of the AFT ages of the samples shows that the Longshoushan experienced significant exhumation during t...
7 Citations Source Cite
Published on Sep 1, 2017in Journal of Asian Earth Sciences 2.87
Tao Wang10
Estimated H-index: 10
,
Ying Tong13
Estimated H-index: 13
+ 9 AuthorsT.V. Donskaya20
Estimated H-index: 20
(Russian Academy of Sciences)
Abstract The widespread occurrence of voluminous granitoids is a typical characteristic of the Central Asian Orogenic Belt (CAOB) in the central and eastern parts of Central Asia. The granitoids occupy a total area more than 8 million km 2 , with three major area peaks at Cambro-Ordovician, Carboniferous-Permian, and Jurassic. Six zircon age peaks at ca. 500, 430–370, 330–300, 290–260, 210–170 and 145–110 Ma. The early Paleozoic granitoids (540–440 Ma, with age peak at ca. 500 Ma) mainly occur i...
8 Citations Source Cite
Published on Sep 1, 2017in Gondwana Research 5.66
De-Bin Yang16
Estimated H-index: 16
(Jilin University),
Hao-Tian Yang2
Estimated H-index: 2
(Jilin University)
+ 2 AuthorsFeng Wang19
Estimated H-index: 19
(Jilin University)
Abstract With the aim of constraining the influence of the surrounding plates on the Late Paleozoic–Mesozoic paleogeographic and tectonic evolution of the southern North China Craton (NCC), we undertook new U–Pb and Hf isotope data for detrital zircons obtained from ten samples of upper Paleozoic to Mesozoic sediments in the Luoyang Basin and Dengfeng area. Samples of upper Paleozoic to Mesozoic strata were obtained from the Taiyuan, Xiashihezi, Shangshihezi, Shiqianfeng, Ermaying, Shangyoufangz...
6 Citations Source Cite
Published on Aug 1, 2017in Journal of Asian Earth Sciences 2.87
Stijn Glorie16
Estimated H-index: 16
(University of Adelaide),
Igor Alexandrov2
Estimated H-index: 2
(Russian Academy of Sciences)
+ 3 AuthorsBor-ming Jahn78
Estimated H-index: 78
(National Taiwan University)
Abstract Sakhalin Island represents a key locality to study the tectonic evolution of the western Pacific. The island is located at the Amur-Okhotsk plate margin and records a complex thermotectonic history. Apatite double dating (U-Pb and fission track) and thermal history modelling were applied to three late Eocene granitoid massifs within central and southern Sakhalin: the Aniva, Okhotsk and Langeri complexes. Apatite U-Pb results yield consistent late Eocene (∼40–37 Ma) ages, suggesting rapi...
19 Citations Source Cite
Published on Jul 1, 2017in Tectonics 3.58
Kelly Thomson1
Estimated H-index: 1
(University of Texas at Austin),
Daniel F. Stockli49
Estimated H-index: 49
(University of Texas at Austin)
+ 2 AuthorsAndrea Fildani29
Estimated H-index: 29
(Statoil)
South central Pyrenean foreland basin fill preserves the eroded remnants of the early stages of fold-thrust belt evolution and topographic growth. Specifically, the Eocene Hecho Group in the Ainsa Basin contains a succession of turbiditic channels and levees deposited in the transition zone between the fluvial-deltaic and deep marine depozones. Detailed isotopic provenance analyses allow for the reconstruction of sediment sources of the ancient sediment routing systems. This study presents 2332 ...
8 Citations Source Cite
Published on Jan 1, 2017in Geological Society of America Bulletin 4.04
Scott Giorgis8
Estimated H-index: 8
(State University of New York System),
John Weber11
Estimated H-index: 11
(Grand Valley State University)
+ 2 AuthorsJames R. Metcalf3
Estimated H-index: 3
(University of Colorado Boulder)
The Central Range fault zone is a continental transform that accommodates most of the present-day slip between the Caribbean and South American plates in Trinidad. Global positioning system data and paleoseismic work suggest that this zone is active today and has been active for at least the past several thousand years. The modern fault zone overprints a middle Miocene fold-and-thrust belt; therefore, the strain recorded in the Central Range fault zone is the sum of both middle Miocene and more ...
3 Citations Source Cite
Tianchen He4
Estimated H-index: 4
(University College London),
Ying Zhou2
Estimated H-index: 2
(University College London)
+ 6 AuthorsGraham A. Shields34
Estimated H-index: 34
(University College London)
New detrital zircon ages confirm that the Neoproterozoic strata of the southeastern North China Craton (NCC) are mostly of early Tonian age, but that the Gouhou Formation, previously assigned to the Tonian, is Cambrian in age. A discordant hiatus of >150–300 myr occurs across the NCC, spanning most of the late Tonian, Cryogenian, Ediacaran and early Cambrian periods. This widespread unconformable surface is akin to the Great Unconformity seen elsewhere in the world and highlights a major shift i...
6 Citations Source Cite
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