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Review of Late Jurassic-early Miocene sedimentation and plate-tectonic evolution of northern California:illuminating example of an accretionary margin

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Chinese Journal Of geochemistry 2015年第2期34卷 123-142页

作者： w.g.ernst Department of geological & Environmental Sciences Stanford University

Production of voluminous igneous arc rocks,high-pressure/low-temperature(HP/LT) metamafic rocks,westward relative migration of the Klamath Mountains province,and U-Pb ages of deposition,sediment sources,and spatial locations of Jurassic and younger,detrital zirconbearing clastic rocks constrain geologic development of the northern California continental edge as follows:(1) At~ 175 Ma,transpressive plate underflow began to generate an Andean-type Klamath-Sierran arc along the margin.(2)Oceanic crustal rocks were metamorphosed under HP/LT conditions in an inboard,east-inclined subduction zone from~ 170-155 *** for the Red Ant blueschists,such Ethologies remained stored at depth;most HP/LT mafic tectonic blocks returned surfaceward only during mid- and Late Cretaceous time,chiefly entrained in circulating,buoyant Franciscan mud-matrix melange.(3) By ~ 165 Ma and continuing to ~ 150-140 Ma,erosion supplied volcanogenic debris to proximal Mariposa-galice ± Myrtle overlap strata.(4) At ~ 140,immediately prior to the onset of paired Franciscan and great Valley group(gVg) +Hornbrook deposition,the Klamath salient was deformed and displaced ~ 100-150 km westward relative to the Sierran arc,stranding pre-existing oceanic crust on the south as the Coast Range Ophiolite(CRO).(5) After the end-ofJurassic seaward step-out of the Farallon-North American convergent plate junction,terrigineous debris began to be deposited in the outboard Franciscan trench and intervening great Valley forearc.(6) Voluminous sedimentation and accretion of Franciscan Eastern + Central belts and gVg detritus took place during paroxysmal igneous activity and rapid,nearly orthogonal plate convergence at^125-80 Ma.(7) Sierran arc volcanism-plutonism ceased by^80 Ma in northern California,signaling a transition to shallow,nearly subhorizontal eastward plate underflow attending Laramide orogeny far to the east.(8) Presently exposed Paleogenelower Miocene Franciscan Coastal Belt sedimentary strata were

关键词：板块构造早中新世加利福尼亚州晚侏罗世增生保证金 U-Pb年龄地层沉积

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Petrochemical Comparison of 3.5 ga Old Mafic Amphibolite Inclusions from Eastern Hebei Province with Archean Mafic-ultramafic Supracrustais of Uncertain Antiquity,Southern Jilin Eastern Liaoning Provinces,China

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Chinese Journal Of geochemistry 1989年第2期8卷 97-111页

作者： w.g.ernst Institute of geophysics and Planetary Physics Department of Earth and Space Sciences University of California Los Angeles California 90024-1567

New major element data for coexisting minerals and bulk-rock REE analyses,combined with previously obtained petrologic/geologic information,allow comparison of Archean mafic-ultramafic meta-igneous rocks from adjacent portions of northeastern Sino-Korean shield .Isotope data published by previous workers document an Early Archean age of formation for metabasaltic rocks now occurring as mafic amphibolite inclusions in tonalitic gneisses west of Bohai Bay(area).Mafic-ultramafic mineral assemblages developed in tonalitic gneisses west of Bohai Bay(areaA).Mafic-ultramafic mineral assemblages developed in amphibolite facies Archean supracrustals east of Bohai Bay(areaB)are chemically similar ,but pre-existing phase associations have been overprinted by the effects of several later metamorphic ***0peridotitic area B protoliths appear to be more magnesian ,averaging-12wt.%MgO(versus-7wt.%for area A),and are slightly less fractionated in REE concentrations relative to chondrites(La-Lu=30-8X versus 37-14X for area A),thus perhaps being more mantle-like than area A metabasaltic *** basaltic-komatiitic series east of Bohai Bay probably represents the most ancient crust of that region,being invaded by Archean tonalities,which were subsequently converted to *** observations are compatible with the hypothesis that ,similar to area A metabasaltic rocks now found as amphibolitic inclusions in orthogneisses,are B mafic supracrustals were formed during Early of Middle Archean time ,prior to widespread isofacial amphibolite facies metamorphism(600-700℃,5-7kb,low αH2O).

关键词：岩石化学辽宁河北闪岩包裹体太古代铁镁质超基性岩地质构造

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High-pressure/low-temperature Metamorphism in Northern Hubei Province,Central China

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资源环境与工程 2016年第B04期30卷 89-104页

作者： g.Zhou Y.J.Liu E.A.Eide J.g.Liou w.g.ernst Hubei Bureau of geology and Mineral Resources Wuhan Hubei 430022 Department of geology Stanford UniversityStanford California 94305

The Qinling-Dabie accretionary fold belt in east-central China represents the E-w trending suture zone between the Sino-Korean and Yangtze cratons. A portion of the accretionary complex exposed in northern Hubei Province contains a high-pressure / low-temperature metamorphic sequence progressively metamorphosed from the blueschist through greenschist to epidote-amphibolite / eclogite facies. The Hongan metamorphic belt can be divided into three metamorphic zones,based on progressive changes in mineral assemblages: Zone Ⅰ,in the south,is characterized by transitional blueschist-greenschist facies; ZoneⅡis characterized by greenschist facies; ZoneⅢ,in the northern most portion of the belt,is characterized by eclogite and epidote-amphibolite facies sequences. Changes in amphibole compositions from south to north as well as the appearance of increasingly higher pressure mineral assemblages toward the north document differences in metamorphic P-T conditions during formation of this belt. Preliminary P-T estimates for Zone I metamorphism are 5 ~ 7 kbar,350 ~ 450℃; estimates for Zone III eclogites are 10 ~ 22 kbar,500 ±50℃. The petrographic,chemical and structural characteristics of this metamorphic belt indicate its evolutionin a northward-dipping subduction zone and subsequent uplift prior to and during the final collisionbetween the Sino-Korean and Yangtze cratons.

关键词： central China eclogite high-P/T belt transitional blueschist-greenschist

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台湾的造山作用与变质作用

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海洋石油 1984年第2期 8-17+37页

作者： w.g.ernst 陈颐亨

台湾的主要部分是由晚古生代一中生代的基底杂岩及不整合上覆的新生代盖层组成的;此岩域沿台湾岛东侧的纵谷与海岸山脉(晚第三纪吕宋火山弧和吕宋海槽弧前盆地的北廷部分)斜接。一次大的热动力变动(造成大南澳片岩岩域)中断了晚古生代... 详细信息

台湾的主要部分是由晚古生代一中生代的基底杂岩及不整合上覆的新生代盖层组成的;此岩域沿台湾岛东侧的纵谷与海岸山脉(晚第三纪吕宋火山弧和吕宋海槽弧前盆地的北廷部分)斜接。一次大的热动力变动(造成大南澳片岩岩域)中断了晚古生代和中生代沿亚洲东部裂陷边缘的冒地槽型砂岩、页岩、灰岩和玄武岩夹层的堆积。此杂岩由西面的太鲁阁带和被推测断层分开的东面的玉里带组成。太鲁阁带北部有闪岩组合出现外,均以黑云母带绿片岩相组合为特征,并伴有S型花岗岩侵位。玉里带缺乏大理岩层和花岗岩侵入体,却含很少的蛇纹岩及绿帘石闪岩和冻兰闪石闪岩的构造透镜体。此晚中生代的大南澳杂岩显然是由亚洲边缘之下的俯冲作用造成的。玉里带的镁铁质构造块体显示出部分地转变成含兰闪石组合;放射性测量的视年龄为8—14百万年。继早第三纪重新发生裂陷和海底扩张之后,沉积了新生代盖层。该盖层多半由覆盖着亚洲大陆边缘的沉积层(加玄武岩)及向海在南中国海中堆积的陆坡沉积组成。而在与逼近的吕宋弧相邻的地带则形成了加积楔,标志着菲律宾海板块无俯冲的西缘。在上新世—更新世海岸山脉与中国硅铝壳碰撞期间,新生代的陆坡单元曾发生叠瓦作用并向西逆冲;在此加载期间压力与温度的增大明显地造成了基底和被动边缘沉积盖层的重结晶。变质作用由西部山麓的成岩相和沸石相到底岩域变为上部绿片岩相。对比之下,分布于纵谷以东的外来岩域却看来实际上并未变质。可是,在海岸山脉不变质的滑乱层沉积中呈碎屑和滑块出现的台东蛇绿岩,却受到了早中新世(?)阳起石角页岩相洋脊重结晶作用的影响,并带有晚中新世—早上新世洋底沸石化的烙印。因而,台湾的造山运动至少包括两个主要的会聚幕:(1)晚中生代古大平洋岩石圈板块向西下潜,造成成对的高温和高压带;(2)紧接着8—14百万年前的隐蔽俯冲事件之后,在南中国海岩石圈向东下降到菲律宾海板块之下期间,有一个上新世—更新世的碰撞事件,它造成了一套成岩到低级变质的层序。一个外侧钙—硷质火山弧的影响进一步使情况更趋复杂。由该年轻造山区的共生次序所显示出的时—空关系表明变质作用和造山过程是错综复杂的。

关键词：晚第三纪海岸山脉变质作用地质作用前新生代造山运动地壳运动造山作用台湾

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根据蓝片岩的退变质压力-温度轨迹推测俯冲带的构造历史

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地质科学译丛 1990年第1期7卷 21-24页

作者： w.g.ernst 张泽明

许多显生宙的会聚板块边界都以出现不连续的具有高压进变质轨迹的蓝片岩带为标志.常见的蓝片岩组合可以发生广泛的绿片岩和(或)绿帘-角闪岩组合的叠加.如西阿尔卑斯.对这种类型的高压变质带来说,退变质作用是非常快速的、近于绝热的降... 详细信息

许多显生宙的会聚板块边界都以出现不连续的具有高压进变质轨迹的蓝片岩带为标志.常见的蓝片岩组合可以发生广泛的绿片岩和(或)绿帘-角闪岩组合的叠加.如西阿尔卑斯.对这种类型的高压变质带来说,退变质作用是非常快速的、近于绝热的降压作用;其中某些地体在降压的早期还经历了连续加热。抬升作用很可能是由于岛弧、大洋高原或陆壳碎块进入了俯冲带(碰撞带),俯冲速度骤降或停止,并由此导致受阻的重结晶俯冲杂岩在浮力的作用下近于绝热上升的结果.另一种类型的高压变质带,如加利福尼亚西部的弗朗西斯科带,保存有变质的文石,没有低压组合的叠加。退变质作用几乎就是沿进变质p-T轨迹回返.或对于原来的高变质级岩块而言,其退变质甚至可以出现于更高的p/T比率下。很显然,部分这种类型的变质带应是在板块连续俯冲和冷却作用进行过程中,受均衡作用的驱使沿俯冲带缓慢抬升的.其上升运动是以构造叠瓦岩片、混杂岩中的层间回流,部分也许是以底垫增生柱的侧向扩张形式进行的.由此可见,高压变质带的退变质p-T轨迹对会聚板块的构造历史可以提供重要的约束条件。

关键词：蓝片岩压力俯冲带构造历史

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Spatial Distribution and Tectonic Evolution of Ultrahigh-P(UHP) and High-P(HP) Metamorphic Belts in Central and Eastern China

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资源环境与工程 2016年第B04期30卷 76-88页

作者： J.g.Liou w.g.ernst Xiaomin wANg Ruyuan ZHANg E.Eide Jun LIU S.Maruyama Leslie Ames gaozhi ZHOU Yuanjun LIU Stanford University Standford California 94305 Tokyo University Komaba 153 - 8902 University of California Senta Barbara 93106 Hubei Bureau geol. Mineral. Resource WuhanHubei 430022

In the Triassic suture between the Sino-Korean and Yangtze cratons,the Qinling-Dabie metamorphic complex includes three tectonic units: a northern migmatitic terrane( P < 20 kb),a central UHP coesite- and diamondbeari... 详细信息

In the Triassic suture between the Sino-Korean and Yangtze cratons,the Qinling-Dabie metamorphic complex includes three tectonic units: a northern migmatitic terrane( P g eclogite belt(20 ~ 40 kb),and a southern HP blueschist-eclogite belt(5 ~ 12 kb). Protoliths include continental basement of late Archean to Proterozoic granitic gneiss complexes,and mid-to late Proterozoic bimodal volcanics,platform carbonates,and turbidite sequences including peraluminous sediments. Some early Paleozoic rocks are included as protoliths in the HP belt. The metamorphic complex is segmented into several large blocks by NE-Sw trending faults. Three( Dabie,Hongan and wudan) occur in central China,and an eastern extension,the Su-Lu block is displaced to the north by the Tanlu fault. The UHP rocks are best exposed in the Dabie and Su-Lu blocks,whereas HP blueschists occur throughout the Hongan and wudan blocks. widespread occurrence of conjugate faults in the metamorphic complex suggests differential doming after tectonic juxtaposition of the UHP and HP units at shallow crustal levels. Eclogites of the UHP belt occur as blocks in ultramafic rocks,marble and gneiss and as thin layers interbedded with gneiss; some contain coesite and coesite pseudomorphs in garnet,omphacite,kyanite and epidote. Microdiamond inclusions in garnet have been reported. C-type glaucophane-bearing eclogites are restricted to the Hongan HP belt and contain paragonite instead of kyanite. The coherent HP terrane displays progressive zonation from transitional blueschist / greenschist,through greenschist and epidote amphibolite to eclogite assemblages. The UHP and HP belts possess similar metamorphic trends,deformation features and record clockwise P-T paths. Disposition of the UHP belt to the north of the HP belt,the northward increase in metamorphic grade,and the southward vergence of structures suggest formation during northward underflow of a microcontinent beneath

关键词： UHP Spatial Distribution and Tectonic Evolution of Ultrahigh-P and High-P HP Metamorphic Belts in Central and Eastern China

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透闪石50-契尔马克分子50+过剩H2O体系压力到10kbar的实验研究

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地球与环境 1988年第8期 52-59+38页

作者：曹荣龙 ,C.Ross ,w.g.ernst ,曲木

对总成分为镁角闪石（2CaO·4MgO·Al2O3·7SiO2）+过剩H2O的体系进行了压力到10kbar的相平衡研究。角闪石稳定的下限温度当1000bar时为519℃,2000 bar时为541℃,10kbar时为718℃。低于下限温度不出现角闪石,体系由低温组合:an+chl+di+t... 详细信息

对总成分为镁角闪石（2CaO·4MgO·Al2O3·7SiO2）+过剩H2O的体系进行了压力到10kbar的相平衡研究。角闪石稳定的下限温度当1000bar时为519℃,2000 bar时为541℃,10kbar时为718℃。低于下限温度不出现角闪石,体系由低温组合:an+chl+di+tc（+f）所组成,除an外少量的铝这时主要进入di和tc中,相邻的高温平衡组合为;amph+an+chl+f,在1000—3000bar较低的压力下,角闪石中铝的固溶量甚低,固体溶液的范围从几乎纯的透闪石到大约cu11tr96ts20,这与绝大多数天然镁角闪石的成分一致。10kbar流体压力下固溶体成分约到cu（08）tr（53）ts41。含铝tr+fo的高温上限温度大体上在化学计量透闪石的脱水曲线以下约20—25℃。含水熔体当10kbar时见于900℃,熔体与角闪石共存的持续温度区间超过60℃。有关实验结果说明了天然界tr和ts之间（?）溶体限于（tr100—70）严格成分范围的原因。

关键词：角闪石固溶体链状硅酸盐矿物 H2O 总成分电子探针微量分析微探针分析电子探针分析辉石化学计量单斜闪石韭闪石流体压力化学组成化学成分人工合成热力学平衡相平衡马克分子实验研究

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A novel method for clustering cellular data to improve classification

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Neural Regeneration Research 2025年第9期20卷 2697-2705页

作者： Diek w.wheeler giorgio A.Ascoli Center for Neural Informatics Structures&PlasticityKrasnow Institute for Advanced Study Bioengineering Department Volgenau School of Engineering george Mason University FairfaxVAUSA

Many fields,such as neuroscience,are experiencing the vast prolife ration of cellular data,underscoring the need fo r organizing and interpreting large datasets.A popular approach partitions data into manageable subsets via hierarchical clustering,but objective methods to determine the appropriate classification granularity are *** recently introduced a technique to systematically identify when to stop subdividing clusters based on the fundamental principle that cells must differ more between than within *** we present the corresponding protocol to classify cellular datasets by combining datadriven unsupervised hierarchical clustering with statistical *** general-purpose functions are applicable to any cellular dataset that can be organized as two-dimensional matrices of numerical values,including molecula r,physiological,and anatomical *** demonstrate the protocol using cellular data from the Janelia MouseLight project to chara cterize morphological aspects of neurons.

关键词： cellular data clustering dendrogram data classification Levene's one-tailed statistical test unsupervised hierarchical clustering

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Quantum Mechanics of a Quasi-Euclidean Space with Planck Length, Rotational Symmetry and Translational Symmetry

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Journal of Applied Mathematics and Physics 2025年第1期13卷 302-326页

作者： Yan Zhou Junyan Zhang ernst Meyer Xingkai Zhang Jing Zhang Lanzhou Institute of Chemical Physics Chinese Academy of Sciences Lanzhou China Department of Physics University of Basel Basel Switzerland

This work is focused on a quasi-Euclidean space with UV cutoff, IR cutoff and symmetries. Mathematical analysis reveals that the UV cutoff results in the minimum structures of space. Dominated by rotational symmetry, the structure should be a local one in situ or on a sphere. Investigations show that a 10D minimum structure is a non-local one with transformability between in-situ state and spherical state due to its special topology. Based on the quantum behaviors of the 10D structure controlled by translational symmetry, IR cutoff determines two long-range interactions with dimensionless constants of ~1/137.036 and ~1/1.628E+38, respectively.

关键词： Planck Length IR Cutoff Symmetry Fine Structure Constant (FSC) Quantum gravity

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Dynamic modeling of a three-dimensional braided composite thin plate considering braiding directions

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Applied Mathematics and Mechanics(English Edition) 2025年第1期46卷 123-138页

作者： Chentong gAO Huiyu SUN Jianping gU w.M.HUANg College of Aerospace Engineering Nanjing University of Aeronautics and Astronautics School of Mechanical and Aerospace Engineering Nanyang Technological University Jiangsu Key Laboratory of Advanced Structural Materials and Application Technology School of Materials Science and EngineeringNanjing Institute of Technology

Currently, there are a limited number of dynamic models available for braided composite plates with large overall motions, despite the incorporation of three-dimensional(3D) braided composites into rotating blade components. In this paper, a dynamic model of 3D 4-directional braided composite thin plates considering braiding directions is established. Based on Kirchhoff's plate assumptions, the displacement variables of the plate are expressed. By incorporating the braiding directions into the constitutive equation of the braided composites, the dynamic model of the plate considering braiding directions is obtained. The effects of the speeds, braiding directions, and braided angles on the responses of the plate with fixed-axis rotation and translational motion, respectively, are investigated. This paper presents a dynamic theory for calculating the deformation of 3D braided composite structures undergoing both translational and rotational motions. It also provides a simulation method for investigating the dynamic behavior of non-isotropic material plates in various applications.

关键词： braiding direction composite thin plate dynamic model large overall motion O313.7 three-dimensional (3D) braided composite

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