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A Deep Mantle Source for the late neoarchean Metamorphosed Basalts in Eastern Hebei,North China Craton:Insights from Whole-Rock Geochemistry and Sm-Nd Isotopes,and Zircon U-Pb-Hf Isotopes

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Journal of Earth Science 2024年第1期35卷 29-40页

作者： Zhuang Li Chunjing Wei Chuan Yang Xi Zhang College of Geosciences China University of PetroleumBeijing 102249China MOE Key Laboratory of Orogenic Belts and Crustal Evolution School of Earth and Space SciencesPeking UniversityBeijing 100871China China Transport Telecommunications and Information Center Beijing 100011China

The basalts within the greenstone belt worldwide serve as an ideal target to decipher the nature of Archean mantle sources and further to extend the understanding of the early stages of Earth's evolution.To provide important insights into the issues,we carried out a detailed investigation of whole-rock geochemistry and Sm-Nd isotopes,and zircon U-Pb-Hf isotopes for the late neoarchean metamorphosed basalts in eastern Hebei,North China Craton.U-Pb isotopic dating using the LA-ICPMS on zircons reveals that the basalts in eastern Hebei erupted at ca.2.48-2.51 Ga and subsequently experienced multiple regional metamorphic events at 2477 and 1798 Ma,respectively.The metamorphosed basalts are featured by low SiO_(2),MgO,K_(2)O+Na_(2)O,and high Fe O contents,endowed with the subalkaline and high-Fe tholeiitic affinities.The radiogenic initial Nd and Hf isotope values and correlations among V,Ni and Cr contents strongly imply that the basalts experienced significant clinopyroxene and olivine fractionation and minor crustal contamination during magma evolution.They are also characterized by the relatively low total REE contents and exhibit significant depletions to moderate enrichments in the LREE contents,indicating the derivation from a deep mantle source in an Archean proto-mantle plume setting.

关键词： zircon U-Pb-Hf isotopes geochemistry late neoarchean basaltic magmatism North China Craton Archean proto-mantle plume

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新太古代末构造体制和古环境的关键转变——独特的共生金属矿床证据

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Science Bulletin 2022年第23期67卷 2438-2448,M0004页

作者：翟明国 State Key Laboratory of Continent Dynamics Northwest UniversityXi'an 710075China State Key Laboratory of Lithospheric Evolution Institute of Geology and GeophysicsChinese Academy of SciencesBeijing 100029China College of Planetary and Earth Science University of Chinese Academy of SciencesBeijing 100049China

在地球特别是大陆演化的历史上,物质的演化是关键证据.岩石是最有效载体和研究对象.我国东北的新太古代条带状铁建造(BIF)和产于火山-泥质岩中的块状Cu-Zn硫化物矿床(VMS-like),提供了氧化矿床和硫化矿床共生的实例.这种独特共生矿床的... 详细信息

在地球特别是大陆演化的历史上,物质的演化是关键证据.岩石是最有效载体和研究对象.我国东北的新太古代条带状铁建造(BIF)和产于火山-泥质岩中的块状Cu-Zn硫化物矿床(VMS-like),提供了氧化矿床和硫化矿床共生的实例.这种独特共生矿床的形成需要构造机制和地球环境条件的双重控制:类似现代板块构造的壳内俯冲和陆壳部分熔融,可以提供成矿元素;频繁的火山喷发导致的光化学等复杂作用使得海水氧化程度发生变化,能够提供成矿的条件.上述构造和古环境的耦合只出现在新太古代末-古元古代初有限的时间段内,延续到大氧化事件的结束(~1.85 Ga).它们的时代~2.5 Ga,正是太古宙与元古宙的分界年龄,指示了地球历史上绝无仅有的巨大变革.

关键词： Co-existing metal deposits late neoarchean Indicator of transition Tectonic regimes Earth’s environments

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Discovery of rhyolitic tuffaceous slate in the southwestern margin of Yangtze Craton:Zircon U-Pb ages(2491 Ma)and tectonic-thermal events

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China Geology 2021年第4期4卷 616-629页

作者： Jun-ping Liu Su-mei Tian Xun-zao Zhu Jin-hua Ma Jing Li Shao-bin Hu Sai-ying Yu Hu Zhang Zhong-ming She Xu-gui Li Yunnan Institute of Geological Survey Kunming 650216China China University of Geosciences Beijing 100083China Key Laboratory of Sanjiang Metallogeny and Resources Exploration and Utilization Ministry of Natural ResourcesKunming 650051China Yunnan Department of Natural Resources Kunming 65000China

The Mesoproterozoic Dongchuan Group that is widely exposed in Yimen area,central Yunnan Province is a series of sedimentary sort of low-grade metamorphic rocks interbedded with volcanic rocks,which are closely related to the early tectonic evolution of the Earth.However,its formation era,sedimentary filling sequence,and geotectonic characteristics have always been in dispute.In this study,several rhyolitic tuffaceous slate interlayers with a centimeter-level thickness were found in the previously determined Heishan Formation of the Dongchuan Group located to the western part of Yimen-Luoci fault zone.This paper focuses on the study of the rhyolitic tuffaceous slate in Qifulangqing Village,Tongchang Township,Yimen County.LA-ICP-MS zircon dating was conducted,achieving the crystallization age of magma of 2491±15 Ma and the metamorphic ages of about 2.3 Ga,2.0 Ga,and 1.8 Ga for the first time.Meanwhile,according to in-situ Hf isotope analysis,the zirconεHf(t)values were determined to range from−3.0 to 7.6,with an average of 2.7.Furthermore,the first-stage Hf model age(TDM1)was determined to be 2513−2916 Ma,indicating that the provenance of the rhyolitic tuffaceous slate is the depleted mantle or juvenile crust between the Middle Mesoarchean and the late neoarchean.Therefore,it is believed that the strata of the slate were deposited in the late neoarchean,instead of the Mesoproterozoic as determined by previous researchers.Accordingly,it is not appropriate to group the strata into the Mesoproterozoic Dongchuan Group.Instead,they should be classified as the Maolu Formation of the neoarchean Puduhe Group given the lithologic association and regional information.Furthermore,the magma ages of 2491±15 Ma are highly consistent with the eras of the large-scale late neoarchean orogenic magmatic activities on the northern margin of the Yangtze Craton,and thus reflect the orogenic process consisting of subduction and collision from late neoarchean to Early Paleoproterozoic.The magmatic activities during this period were possib

关键词： Maolu Formation Puduhe Group late neoarchean Zircon U-Pb age Tectonic-thermal event Geological survey engineering Eastern margin of Qinghai-Tibet Plateau Yangtze Craton

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