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Structural Control of the Getang Carlin-Type Gold Deposit in Southwest China

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Journal of Earth Science 2024年第2期35卷 536-552页

作者： Guoping Zeng Xinlu Hu Diwei Luo jianzhong liu Shuzhen Yao Yongjie Jin Wuhan Center China Geological SurveyWuhan430205China Central South China Innovation Center for Geosciences Wuhan430205China Faculty of Earth Resources China University of GeosciencesWuhan430074China Geological Party 105 Guizhou Bureau of Geology and Mineral Exploration&DevelopmentGuiyang550018China

The Getang is a representative Carlin-type gold deposit in Southwest *** has a proven reserve of about 30 tonnes at an average grade of 5.1 g/t *** orebodies occur as strat-abound lenses,and are structurally controlled by shallow NWW-and NE-trending fold-fault systems and the unconformity between the Upper and Middle *** this study,the regional-and deposit-scale structural investigations,joints and finite strain measurements,and stress and dynamic analysis were conducted with an aim to reveal the structural process of the Getang gold deposit and clarify the relationship between the gold mineralization and *** phases of deformation were identified in the deposit:(1)paleokarst was generated by a crustal uplift when the Youjiang Basin experienced extension at the end of the Middle Permian,laying the foundation for the unconformity;(2)the NW-trending structures were formed under a NNE-SSW compression during the Indochina-South China collision(Indosinian orogeny)in Triassic;(3)the NE-trending structures were generated or reactivated under a NW-SE-oriented compression during the Yanshanian intracontinental *** unconformity recorded two episodes of tectonic evolution in the NNE-SSW and NW-SE *** analyses and geochronology data suggest that the Getang gold deposit was formed as a result of tectonic transition from compression to extension during the Yanshanian intracontinental orogeny.

关键词： Carlin-type gold deposit structural features finite strain Getang Southwest China economy geology geochemistry

A lunar time scale from the perspective of the Moon’s dynamic evolution

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Science China Earth Sciences 2024年第1期67卷 234-251页

作者： Dijun GUO jianzhong liu James WHEAD Fuqin ZHANG Zongcheng LING Shengbo CHEN Jianping CHEN Xiaozhong DING Jinzhu JI Ziyuan OUYANG State Key Laboratory of Space Weather National Space Science CenterChinese Academy of SciencesBeijing 100190China Center for Lunar and Planetary Sciences Institute of GeochemistryChinese Academy of SciencesGuiyang 550081China Department of Earth Environmental and Planetary SciencesBrown UniversityProvidence RI 02912USA Institute of Geology and Geophysics Chinese Academy of SciencesBeijing 100029China Shandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment Institute of Space SciencesShandong UniversityWeihai 264209China College of Geoexploration Science and Technology Jilin UniversityChangchun 130026China School of Earth Sciences and Resources China University of GeosciencesBeijing 100083China Institute of Geology Chinese Academy of Geological SciencesBeijing 100037China School of Resources and Environmental Engineering Inner Mongolia University of TechnologyHohhot 010051China Center for Excellence in Comparative Planetology Chinese Academy of SciencesHefei 230026China

A geologic time scale is a chronological system that separates the geological strata of a planetary body into different units in temporal sequence and shows its progressive *** time scale of the Moon was established a half-century ago during the telescopic-early Apollo exploration era,using data with limited spatial coverage and *** past decades have seen a wide array of studies,which have significantly extended our understanding of global lunar geologic *** on a comprehensive review of lunar evolution with respect to the dynamical changes,we propose two major updates to the current lunar time scale paradigm to include the evolution of both endogenic and exogenic dynamic forces now known to have influenced early lunar ***,based on the temporal interplay of exogenic and endogenic processes in altering the Moon,we defined three Eon/Eonothem-level units to represent three dynamical evolutionary ***,the pre-Nectarian System is redefined and divided as the magma ocean-era Magma-oceanian System and the following Aitkenian System beginning with the South Pole-Aitken *** ejecta of this basin,Das Formation,was deposited on the primordial lunar crust as the oldest stratum produced from exogenic *** updated lunar time scale,facilitated by the post-Apollo exploration and research advances,provides an integrated framework to depict the evolution of the Moon and has important implications for the geologic study of other terrestrial planets.

关键词： The Moon Geologic time scale Evolution history Endogenic process Exogenic process

Latest Scientific Results of China's Lunar and Deep Space Exploration(2022–2024)

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空间科学学报 2024年第4期44卷 622-632页

作者： XU Lin LI Lei liu jianzhong LIN Honglei LI Yang liu Yang XIE Lianghai ZHANG Jinhai QIAO Fuhao HAN Juanjuan ZOU Yongliao General Office of the Lunar and Deep Space Exploration Chinese Academy of SciencesBeijng 100190 State Key Laboratory of Space Weather National Space Science CenterChinese Academy of SciencesBeijing 100190 Institute of Geochemistry Chinese Academy of SciencesGuiyang 550081 Institute of Geology and Geophysics Chinese Academy of SciencesBeijing 100029

China has successfully launched six lunar probes so *** Chang'E-1 to Chang'E-4,they completed the circling,landing and roving exploration,of which Chang'E-4 was the first landing on the far side of the Moon in human ***'E-5 was launched in December 2020,bringing back 1731 g of lunar soil *** the detailed analysis of the samples,the scientists understand the history of late lunar volcanism,specifically extending lunar volcanism by about 800 million to 1 billion years,and proposed possible *** addition,there are many new understandings of space weathering such as meteorite impacts and solar wind radiation on the ***'s first Mars exploration mission Tianwen-1 was successfully launched in July *** the study of scientific data,a number of important scientific achievements have been made in the topography,water environment and shallow surface structure of *** paper introduces the main scientific achievements of Chang'E-4,Chang'E-5 and Tianwen-1 in the past two years,excluding technical and engineering *** to the large number of articles involved,this paper only introduces part of the results.

关键词： Lunar and deep space exploration of China Chang’E-4 mission Chang’E-5 mission Tianwen-1 mission

Scientific objectives and payload configuration of the Chang'E-7 mission

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National Science Review 2024年第2期11卷 285-300页

作者： Chi Wang Yingzhuo Jia Changbin Xue Yangting Lin jianzhong liu Xiaohui Fu Lin Xu Yun Huang Yufen Zhao Yigang Xu Rui Gao Yong Wei Yuhua Tang Dengyun Yu Yongliao Zou State Key Laboratory of Space Weather National Space Science Center Chinese Academy of Sciences National Space Science Center Chinese Academy of Sciences Institute of Geology and Geophysics Chinese Academy of Sciences Institute of Geochemistry Chinese Academy of Sciences Shandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment School of Space Science and Physics Institute of Space SciencesShandong University Institute of Drug Discovery Technology Ningbo University State Key Laboratory of Isotope Geochemistry Guangzhou Institute of Geochemistry Chinese Academy of Sciences School of Earth Science and Engineering Sun Yat-sen University Lunar Exploration and Space Engineering Center China Aerospace Science and Technology Corporation

As the cornerstone mission of the fourth phase of the Chinese Lunar Exploration Program, Chang'E-7(CE-7) was officially approved, and implementation started in 2022, including a main probe and a communication relay satellite. The main probe, consisting of an orbiter, a lander, a rover and a mini-flying probe, is scheduled to be launched in 2026. The lander will land on Shackleton crater's illuminated rim near the lunar south pole, along with the rover and mini-flying probe. The relay satellite(named Queqiao-2) will be launched in February 2024 as an independent mission to support relay communication during scientific exploration undertaken by Chang'E-4, the upcoming Chang'E-6 in 2024 and subsequent lunar *** CE-7 mission is mainly aimed at scientific and resource exploration of the lunar south pole. We present CE-7's scientific objectives, the scientific payloads configuration and the main functions for each scientific payload with its key technical specifications.

关键词： Chang’ E-7 scientific objectives scientific payloads

Return to the Moon:New perspectives on lunar exploration

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Science Bulletin 2024年第13期69卷 2136-2148页

作者： Yangting Lin Wei Yang Hui Zhang Hejiu Hui Sen Hu Long Xiao jianzhong liu Zhiyong Xiao Zongyu Yue Jinhai Zhang Yang liu Jing Yang Honglei Lin Aicheng Zhang Dijun Guo Sheng Gou Lin Xu Yuyang He Xianguo Zhang Liping Qin Zongcheng Ling Xiongyao Li Aimin Du Huaiyu He Peng Zhang Jinbin Cao Xianhua Li Key Laboratory of Earth and Planetary Physics Institute of Geology and GeophysicsChinese Academy of SciencesBeijing 100029China State Key Laboratory for Mineral Deposits Research and School of Earth Sciences and Engineering Nanjing UniversityNanjing 210023China State Key Laboratory of Geological Processes and Mineral Resources School of Earth SciencesChina University of GeosciencesWuhan 430074China Institute of Geochemistry Chinese Academy of SciencesGuiyang 550002China Planetary Environmental and Astrobiological Research Laboratory School of Atmospheric SciencesSun Yat-sen UniversityZhuhai 519082China National Space Science Center Chinese Academy of SciencesBeijing 100190China Deep Space Exploration Laboratory/CAS Key Laboratory of Crust-Mantle Materials and Environments University of Science and Technology of ChinaHefei 230026China Shandong Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment Institute of Space SciencesShandong UniversityWeihai 264209China Technology and Engineering Center for Space Utilization Chinese Academy of SciencesBeijing 100094China School of Space and Environment Beihang UniversityBeijing 100191China

Lunar exploration is deemed crucial for uncovering the origins of the Earth-Moon system and is the first step for advancing humanity’s exploration of deep *** the past decade,the Chinese Lunar Exploration Program(CLEP),also known as the Chang’e(CE)Project,has achieved remarkable *** has successfully developed and demonstrated the engineering capability required to reach and return from the lunar ***,the CE Project has made historic firsts with the landing and on-site exploration of the far side of the Moon,along with the collection of the youngest volcanic samples from the Procellarum KREEP *** achievements have significantly enhanced our understanding of lunar *** on this success,China has proposed an ambitious crewed lunar exploration strategy,aiming to return to the Moon for scientific exploration and *** plan encompasses two primary phases:the first crewed lunar landing and exploration,followed by a thousand-kilometer scale scientific expedition to construct a geological cross-section across the lunar *** the limitations of current lunar exploration efforts and China’s engineering and technical capabilities,this paper explores the benefits of crewed lunar exploration while leveraging synergies with robotic *** study refines fundamental lunar scientific questions that could lead to significant breakthroughs,considering the respective engineering and technological *** research lays a crucial foundation for defining the objectives of future lunar exploration,emphasizing the importance of crewed missions and offering insights into potential advancements in lunar science.

关键词： Crewed lunar exploration Water and volatiles Composition and structure of lunar interior Volcanic activity and evolution of lunar mantle Space weathering and radiation environments Exploration technology

沉默大豆GmWRKY33B基因导致大豆抗病性降低

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生物工程学报 2024年第1期40卷 163-176页

作者：钟晨丽王文絮廖莉娜刘建中浙江师范大学生命科学学院浙江金华321004 浙江师范大学生命科学学院浙江省特色经济植物生物技术重点实验室浙江金华321004

WRKY转录因子基因家族是植物特有的转录因子,在防御中起着重要作用。通过生物信息学分析,本研究在古四倍体大豆(Glycine max)基因组中找到一对同源性高达93%的WRKY33同源基因,并将其命名为GmWRKY33B。从GmWRKY33B的两个同源基因保守区... 详细信息

WRKY转录因子基因家族是植物特有的转录因子,在防御中起着重要作用。通过生物信息学分析,本研究在古四倍体大豆(Glycine max)基因组中找到一对同源性高达93%的WRKY33同源基因,并将其命名为GmWRKY33B。从GmWRKY33B的两个同源基因保守区域选取一个315bp片段构建至菜豆豆荚斑驳病毒(bean pod mosaic virus,BPMV)沉默载体(BPMV-VIGS)上,以期同时沉默上述2个GmWRKY33B基因。结果表明,同时沉默2个GmWRKY33B基因并不显著改变沉默植株的表型,但却显著降低了大豆对大豆斑点病菌以及大豆花叶病毒的抗性,说明GmWRKY33B在大豆免疫反应中起正调控作用。激酶分析表明,GmWRKY33B沉默植株中flg22诱导的GmMPK6的磷酸化水平较空载体BPMV-0植株显著降低,说明GmWRKY33B可以通过调控GmMPK6的激酶活性而参与大豆的免疫反应。抗毒素为大豆中主要起防御作用的植保素,而大豆异黄酮类特异性异戊烯基转移酶(prenyltransferase,PT)基因家族是参与大豆抗毒素生物合成的主要基因,许多PT基因启动子区含有与WRKY特异性结合的W-box序列。在丁香假单胞菌pv.甘氨酸(Pseudomonas syringae ***,Psg)侵染条件下,4个PT基因的表达水平在沉默株系中显著降低,说明GmWRKY33B参与PT基因的转录激活。综上所述,GmWRKY33B通过调控GmMPK6的激活以及调控大豆抗毒素生物合成途径中关键酶编码基因的表达而参与免疫反应。

关键词： GmWRKY33 利用病毒诱导基因沉默免疫反应 GmMPK3/6 异戊烯基转移酶大豆抗毒素

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右江盆地卡林型金矿成矿年代学研究进展

地学前缘 2024年第1期31卷 267-283页

作者：高伟胡瑞忠李秋立刘建中李献华中国科学院地球化学研究所矿床地球化学国家重点实验室贵州贵阳550081 中国科学院地质与地球物理研究所岩石圈演化国家重点实验室北京100029 贵州省地质矿产开发局贵州贵阳550081 中国科学院大学地球与行星科学学院北京100049

右江盆地是全球仅次于美国内华达地区的第二大卡林型金矿床集中分布区。由于成矿时代的不确定性,盆地内卡林型金矿床的成矿动力学背景一直不清。为准确确定这些金矿床的成矿时代,近四十年来国内外矿床学家进行了孜孜不倦的探索,从早期... 详细信息

右江盆地是全球仅次于美国内华达地区的第二大卡林型金矿床集中分布区。由于成矿时代的不确定性,盆地内卡林型金矿床的成矿动力学背景一直不清。为准确确定这些金矿床的成矿时代,近四十年来国内外矿床学家进行了孜孜不倦的探索,从早期以石英裂变径迹和流体包裹体Rb-Sr等时线法为代表的定年,到中期以硫化物Re-Os等时线法为代表的单矿物溶样法定年,再到最新以热液金红石、独居石和磷灰石U-Th-Pb法为代表的微区原位定年,其定年对象和方法见证了同位素地质年代学的发展历程。现已基本明确,右江盆地主要发育两期卡林型金矿成矿作用,分别为215~200 Ma和155~140 Ma,相当于印支期和燕山期,其动力学背景分别对应于印支-华南-华北地块碰撞后的印支期陆内造山过程以及燕山期软流圈上涌诱发的岩石圈伸展作用。

关键词：右江盆地卡林型金矿成矿时代印支期和燕山期成矿

沉默大豆GmATG5加速叶片衰老并增强大豆抗病性

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生物工程学报 2024年第4期40卷 1065-1075页

作者： Said M.Hashimi 黄敏君陈宇刘建中浙江师范大学生命科学学院浙江金华321004 浙江师范大学生命科学学院遗传与发育生物学研究所浙江金华321004 浙江师范大学生命科学学院浙江省特色经济植物生物技术重点实验室浙江金华321004

自噬在生物体细胞内物质循环利用及适应各种胁迫方面起着重要作用。然而,对大豆自噬途径的研究鲜有报道。本研究利用大豆豆荚斑驳病毒(bean pod mottle virus,BPMV)介导的基因沉默技术,对大豆自噬相关基因5(autophagy-related gene 5,AT... 详细信息

自噬在生物体细胞内物质循环利用及适应各种胁迫方面起着重要作用。然而,对大豆自噬途径的研究鲜有报道。本研究利用大豆豆荚斑驳病毒(bean pod mottle virus,BPMV)介导的基因沉默技术,对大豆自噬相关基因5(autophagy-related gene 5,ATG5)同源基因进行沉默。结果发现,经暗处理的GmATG5沉默植株叶片上积累过量的ATG8蛋白,说明自噬降解途径受损;与自噬途径受损相一致,暗处理的GmATG5沉默植株叶片出现明显的衰老加速的表型;另外,GmATG5沉默植株叶片中活性氧(reactive oxygen species,ROS)的积累量以及水杨酸含量显著增加,说明沉默GmATG5激活了免疫反应;抗病性分析表明,GmATG5沉默植株对大豆斑点病菌(Pseudomonas syringae ***,Psg)的抗性较空载体对照植株显著增强,但该抗病性的增强并不依赖于丝裂原活化蛋白激酶(mitogen-activated protein kinase,MAPK)途径的激活。

关键词：自噬病毒诱导的基因沉默免疫反应丝裂原活化蛋白激酶(MAPK)

大豆AGB1同源基因在防御反应中起正向调控作用

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生物工程学报 2024年第4期40卷 1050-1064页

作者：吴楠兰胡娇黄敏君王文絮刘建中浙江师范大学生命科学学院浙江金华321004 浙江师范大学生命科学学院浙江省特色经济植物生物技术重点实验室浙江金华321004

由Gα、Gβ和Gγ这3个亚基组成的异源三聚体GTP结合蛋白(简称G蛋白)在真核生物的信号转导中起着重要作用。拟南芥基因组中仅有1个Gβ亚基编码基因AGB1,在免疫反应中起着正调控作用,然而AGB1在大豆防御中的作用尚不清楚。鉴于大豆是四倍... 详细信息

由Gα、Gβ和Gγ这3个亚基组成的异源三聚体GTP结合蛋白(简称G蛋白)在真核生物的信号转导中起着重要作用。拟南芥基因组中仅有1个Gβ亚基编码基因AGB1,在免疫反应中起着正调控作用,然而AGB1在大豆防御中的作用尚不清楚。鉴于大豆是四倍体植物,存在基因功能冗余,本研究利用菜豆豆荚斑驳病毒诱导的基因沉默技术同时沉默大豆基因组中同源性高达86%−97%的4个GmAGB1同源基因,以探究其在大豆免疫中的作用。沉默GmAGB1导致大豆植株出现矮化表型,暗示GmAGB1可能参与大豆的生长发育;抗病性分析表明沉默GmAGB1导致大豆对大豆斑疹病菌的抗性降低,而该抗性的降低与GmAGB1沉默植株叶片中病原菌侵染诱导的活性氧的积累量的显著下降以及细菌中保守的鞭毛蛋白N端22个氨基酸小肽flg22诱导的GmMPK3激活程度的显著降低相关联。此外,酵母双杂交实验证明大豆中的GmAGB1可能与GmAGG1存在互作关系。综上所述,GmAGB1是大豆防御反应中的正调控因子,且大豆中G蛋白也可能以进化上保守的异源三聚体的形式发挥作用。

关键词： GmAGB1 G蛋白病毒诱导的基因沉默技术防御反应活性氧