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High-resolution chronostratigraphy of late Mesozoic sequences in northern North China: Implications for the linkages among intracontinental orogeny, volcanism, Jehol Biota, and Pacific plate subduction
Ma, Qiang1,2,3; Zhong, Yuting2,3,4; Yin, Qingzhu5; Huyskens, Magdalena H.5; Ma, Liang2,3,4; Xia, Xiaoping2,3; Meng, Qing-Ren6; Zhou, Zhong-He7; Xu, Yi-Gang2,3,4
2024
发表期刊GEOLOGY
ISSN0091-7613
卷号52期号:1页码:45-50
通讯作者Ma, Qiang(maqiang@cug.edu.cn) ; Xu, Yi-Gang(yigangxu@gig.ac.cn)
摘要Subduction of the paleo-Pacific plate during the late Mesozoic is thought to have been responsible for the destruction of the North China craton, manifested by intense volcanism, lithospheric deformation, and dramatic changes in surface morphology and terrestrial ecosystems. However, the timing and correlations of these consequential events remain obscure. This issue was addressed here by carrying out a high -resolution geochronologic study on the Upper Jurassic-Lower Cretaceous sequences of the Luanping basin, northern Hebei Province, China. Secondary ion mass spectrometry (SIMS) and chemical abrasion-isotope dilution-isotope ratio mass spectrometry (CA-ID-IRMS) zircon U-Pb ages from samples near the boundaries of the stratigraphic units help to redefine the chronostratigraphic framework of this basin and more importantly reveal that the second phase of the Yanshanian orogeny, representing a tectonic transition from flat to steep subduction of the paleo-Pacific plate, occurred within 0.87 +/- 0.10 m.y. between 134.162 +/- 0.091 Ma and 133.295 +/- 0.043 Ma. Crustal extension then followed and resulted in development of rift basins and vigorous volcanism. The Jehol Biota came into being in Lower Cretaceous successions formed after ca. 130 Ma. The late Mesozoic Luanping basin therefore records how the subduction of the paleo-Pacific plate drove intracontinental orogeny, volcanism, basin development, and ecosystem evolution.
DOI10.1130/G51535.1
关键词[WOS]DESTRUCTION ; CRATON ; LITHOSPHERE
收录类别SCI
语种英语
资助项目National Natural Science Foundation of China[42288201] ; National Natural Science Foundation of China[41973050] ; National Natural Science Foundation of China[42322205] ; National Natural Science Foundation of China[41873018]
项目资助者National Natural Science Foundation of China
WOS研究方向Geology
WOS类目Geology
WOS记录号WOS:001186997700008
出版者GEOLOGICAL SOC AMER, INC
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/23606
专题中国科学院古脊椎动物与古人类研究所
通讯作者Ma, Qiang; Xu, Yi-Gang
作者单位1.China Univ Geosci, Sch Earth Sci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
2.Chinese Acad Sci, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
3.Chinese Acad Sci, Guangzhou Inst Geochem, Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China
4.Southern Marine Sci & Engn Guangdong Lab, Guangzhou 511458, Peoples R China
5.Univ Calif Davis, Dept Earth & Planetary Sci, Davis, CA 95616 USA
6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
7.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China
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GB/T 7714
Ma, Qiang,Zhong, Yuting,Yin, Qingzhu,et al. High-resolution chronostratigraphy of late Mesozoic sequences in northern North China: Implications for the linkages among intracontinental orogeny, volcanism, Jehol Biota, and Pacific plate subduction[J]. GEOLOGY,2024,52(1):45-50.
APA Ma, Qiang.,Zhong, Yuting.,Yin, Qingzhu.,Huyskens, Magdalena H..,Ma, Liang.,...&Xu, Yi-Gang.(2024).High-resolution chronostratigraphy of late Mesozoic sequences in northern North China: Implications for the linkages among intracontinental orogeny, volcanism, Jehol Biota, and Pacific plate subduction.GEOLOGY,52(1),45-50.
MLA Ma, Qiang,et al."High-resolution chronostratigraphy of late Mesozoic sequences in northern North China: Implications for the linkages among intracontinental orogeny, volcanism, Jehol Biota, and Pacific plate subduction".GEOLOGY 52.1(2024):45-50.
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