检索结果-南通市图书馆

Petrogenesis a.d tectonic implica.ions of Ea.ly Creta.eous a.desitic-da.itic rocks,western Qinling(Centra. China.:Geochronologica. a.d geochemica. constra.nts

引用

Geoscience Frontiers 2019年第4期10卷 1507-1520页

作者： Feifei Zha.g peter a. cawood Yunpeng Dong Yuejun Wa.g Sta.e Key La.ora.ory of Continenta. Dyna.ics Department of GeologyNorthwest UniversityXi’an 710069China Depa.tment of Ea.th Sciences University of St.AndrewsNorth StreetSt.Andrews KY16 9ALUK School of Ea.th Atmosphere and EnvironmentMonash UniversityMelbourneVictoria 3800Australia Gua.gdong Provincia. Key La. of Geodyna.ics a.d Geoha.a.ds School of Earth Sciences and EngineeringSun Yat-sen UniversityGuangzhou 510275China

40a./39a. a.d zircon U-Pb geochronologica. a.d whole-rock geochemica. a.a.yses for the La.za.ggou intermedia.e-a.idic volca.ic rocks from the western Qinling orogenic belt,Centra. China.constra.n their petrogenesis a.d the na.ure of the La.e Mesozoic lithospheric *** volca.ic rocks yield hornblende or whole-rock 40a./39a. pla.ea. a.es of 128.3-129.7 Ma.a.d zircon U-Pb a.e of131.3±1.3 *** exhibit SiO2 of 56.86-66.86 wt.%,K2 O of 0.99-2.46 wt.%a.d MgO of 1.03-4.47 wt.%,with Mg#of *** a.e cha.a.terized by a.c-like geochemica. signa.ures with significa.t enrichment in LILE a.d LREE a.d depletion in *** the sa.ples ha.e enriched Sr-Nd isotopic compositions with initia. 87Sr/86Sr ra.ios ra.ging from 0.7112 to 0.7149 a.dεNd(t)va.ues from 10.2 to *** geochemica. signa.ures suggest tha. these volca.ic rocks were derived from enriched lithospherederived ma.ma.followed by the a.simila.ion a.d fra.tiona. crysta.liza.ion(a.C)*** genera.ion of the enriched lithospheric ma.tle is likely rela.ed to the modifica.ion of sediment-derived fluid in response to the Tria.sic subduction/collision event in Qinling orogenic *** ea.ly Creta.eous deta.hment of the lithospheric root provides a.rea.ona.le mecha.ism for understa.ding the petrogenesis of the La.za.ggou volca.ic sequence in the western Qinling orogenic belt.

关键词： 40a./39a. a.d zircon U-Pb geochronology Sr-Nd isotopes Ea.ly Creta.eous a.C process Continenta. lithospheric ma.tle Western Qinling orogenic belt

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

Unta.gling the history of oroclines a.d mounta.n belts

引用

Na.iona. Science Review 2022年第5期9卷 179-180页

作者： peter a.cawood School of Ea.th Atmosphere and Environment Monash University

Oro clines a.e ma.-view bends of the Ea.th’s lithosphere formed by rota.ion of origina.ly qua.ilinea. linea. rock units a.out a.sub-vertica. a.is [1].They ca. ha.e a.plitudes a.d wa.elengths on the order of hundreds of kilometres a.d a.e a.significa.t fea.ure of ma.y a.tive a.d a.cient mounta.n belts(Fig.1,*** orocline,Bolivia. orocline,Betic-Rif Belt,

关键词：

来源：

同方期刊数据库评论

在线全文

同方期刊数据库

学校读者我要写书评

暂无评论

Ra.es of genera.ion a.d growth of the continenta. crust

引用

Geoscience Frontiers 2019年第1期10卷 165-173页

作者： Chris Ha.kesworth peter a.cawood Bruno Dhuime School of Ea.th Sciences University of Bristol School of Ea.th Atmosphere and Environment Monash University CNRS-UMR 5243 Géosciences Montpellier Université de Montpellier

Models for when a.d how the continenta. crust wa. formed a.e constra.ned by estima.es in the ra.es o crusta. growth. The record of events preserved in the continenta. crust is heterogeneous in time with distinctive pea.s a.d troughs of a.es for igneous crysta.lisa.ion, meta.orphism, continenta. ma.gin a.d minera.isa.ion. For the most pa.t these a.e globa. signa.ures, a.d the pea.s of a.es tend to b a.socia.ed with periods of increa.ed reworking of pre-existing crust, reflected in the Hf isotope ra.ios o zircons a.d their eleva.ed oxygen isotope ra.ios. Increa.ed crusta. reworking is a.tributed to periods o crusta. thickening a.socia.ed with compressiona. tectonics a.d the development of supercontinents Ma.ma.types simila. to those from recent within-pla.e a.d subduction rela.ed settings a.pea. to ha. been genera.ed in different a.ea. a. broa.ly simila. times before ~3.0 Ga. It ca. be difficult to put th results of such deta.led ca.e studies into a.more globa. context, but one a.proa.h is to consider when pla.e tectonics beca.e the domina.t mecha.ism involved in the genera.ion of juvenile continenta. crust The development of crusta. growth models for the continenta. crust a.e discussed, a.d a.number o models ba.ed on different da.a.sets indica.e tha. 65%-70% of the present volume of the continenta. crus wa. genera.ed by 3 Ga. Such estima.es ma. represent minimum va.ues, but since ~3 Ga.there ha. been reduction in the ra.es of growth of the continenta. crust. This reduction is linked to a. increa.e in th ra.es a. which continenta. crust is recycled ba.k into the ma.tle, a.d not to a.reduction in the ra.es a.which continenta. crust wa. genera.ed. Pla.e tectonics results in both the genera.ion of new crust a.d it destruction a.ong destructive pla.e ma.gins. Thus, the reduction in the ra.e of continenta. crusta. growth a. ~3 Ga.is ta.en to reflect the period in which pla.e tectonics beca.e the domina.t mecha.ism b which new continenta. crust wa. genera.ed.

关键词： Continenta. crust growth curves Ra.es of crusta. growth Tectonics

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

Pre-Cryogenia. integra.ive stra.igra.hy,biota.,a.d pa.eogeogra.hica. evolution of the Qingha.-Tibeta. Pla.ea. a.d its surrounding a.ea.

引用

Science China.Ea.th Sciences 2024年第4期67卷 899-918页

作者： Peiyua. HU Qingguo ZHa. Guochun ZHa. peter a.cawood Yue Ta.G Yiming LIU Institute of Geology Chinese Academy of Geological SciencesBeijing 100037China Depa.tment of Ea.th Sciences University of Hong KongPokfulam RoadHong Kong 999077China Sta.e Key La.ora.ory of Continenta. Dyna.ics Department of GeologyNorthwest UniversityXi’an 710069China School of Ea.th Atmosphere&EnvironmentMonash UniversityMelbourneVIC 3800Australia

The composition a.d geologica. evolution of pre-Cryogenia. ma.eria. in the Tibeta. Pla.ea. a.d its surrounding a.ea. ha.e pla.ed a. importa.t role in studying the forma.ion a.d evolution of ea.ly supercontinents on *** pa.er systema.ica.ly summa.izes the cha.a.teristics of pre-Cryogenia. sedimenta.ion,pa.eontology,ma.ma.ism,a.d meta.orphism in the Tibeta. Pla.ea. a.d its surrounding *** on existing da.a.the records of pre-Cryogenia. sedimenta.ion a.d pa.eontology a.e ma.nly concentra.ed in the Meso-Neoproterozoic,with rela.ively few records from the Pa.eoproterozoic or *** oldest geologica. record is the Ha.ea. detrita. zircons in the meta.orphosed sedimenta.y rocks of the Hima.a.a.a.d Qa.do a.ea.(ca.4.0 Ga..The Tibeta. Pla.ea. a.d surrounding a.ea. preserve records rela.ed to the forma.ion a.d evolution of the Kenor supercra.on,a.d the Columbia.Rodinia.a.d Gondwa.a.***-Cryogenia. ba.ements ca. be divided into three types:Ta.im-,Ya.gtze-,a.d *** Ta.im-type ba.ement ha. a.pa.eogeogra.hic a.finity with the northern ma.gins of the a.stra.ia. a.d India. continents a.d la.ks detrita. zircon a.e pea.s a.d ma.ma.ic-meta.orphic records rela.ed to the Rodinia.a.sembly(ca.1.3-0.9 Ga..The Ya.gtze-type ba.ement records volca.ic a.tivity rela.ed to globa. cooling in the la.est pre-Cryogenia. period a.d conta.ns Meso-Neoproterozoic stroma.olite a.d micropa.eoflora.fossils,a. well a. ma.ma.icmeta.orphic records rela.ed to Rodinia.a.sembly(ca.1.1-1.0 Ga..The Lha.a.type ba.ement is cha.a.terized by Neoproterozoic rift-rela.ed sediment records(ca.900 Ma.a.d high-pressure meta.orphic events(ca.650 Ma.,with a.prominent pea. of detrita. zircon a.es of ca.1.2-1.1 *** is likely to ha.e a.pa.eogeogra.hic a.finity with the a.rica. continent.

关键词： Tibeta. Pla.ea. Pre-Cryogenia. Sedimenta.ion Fossils Pa.eogeogra.hic evolution

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

Meta.orphic rocks a.d pla.e tectonics

引用

Science Bulletin 2020年第12期65卷 968-969,M0003页

作者： peter a.cawood School of Ea.th a.mosphere a.d Environment.Mona.h University MelbourneVic 3800Australia

Our pla.et is a.dyna.ic system whose evolution ha. been controlled by complex feedba.ks between its solid a.d surficia. components(e.g.,ma.tle,crust,ocea.s,a.mosphere a.d biosphere),a.ross a.ra.ge of tempora. a.d spa.ia. *** the modern Ea.th,these intera.tions a.e controlled by pla.e tectonics,which involves the horizonta. motion of surfa.e pla.es(i.e.,continenta. drift a.d sea.floor sprea.ing)a.ross a.series of continuous linked bounda.ies[1].

关键词：板块构造 ma.tle Ea.th

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

山西五台山-恒山地区晚太古-早元古代若干关键地质问题的再认识:单颗粒锆石离子探针质谱年龄提出的地质制约

引用

地质科学 2000年第2期35卷 175-184页

作者：王凯怡郝杰 Simon Wilde peter cawood 中国科学院地质研究所岩石圈构造演化开放研究实验室北京100029 School of a.plied Geology Curtin University of Technology

大量准确度很高的单颗粒锆石迅谱 (SHRIMP)年代学数据表明 ,五台山 -恒山绿岩带形成于 2 50 0 Ma.前 ,五台山 -恒山绿岩带形成后即与较老的阜平块体拼合。因此 ,该过程中有大量火山 ,深成活动及变质作用 ,是一次重要的造山运动。在 1 8... 详细信息

大量准确度很高的单颗粒锆石迅谱 (SHRIMP)年代学数据表明 ,五台山 -恒山绿岩带形成于 2 50 0 Ma.前 ,五台山 -恒山绿岩带形成后即与较老的阜平块体拼合。因此 ,该过程中有大量火山 ,深成活动及变质作用 ,是一次重要的造山运动。在 1 80 0 Ma.前 ,本区还经历了一次明显的构造热事件 ,主要表现为在地壳较深水平上大规模的冲断作用 ,使原来为不同地壳水平的块体处于同一地壳水平。本文还对原五台群下部层位板峪口组和金岗库组的归属及铁堡不整合面提出了新的看法。

关键词：晚太古代早元古代单颗粒锆石地质年龄

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

地球演化历史中氧逸度变化对壳幔循环启动、风化和超大陆循环的指示

引用

Science Bulletin 2024年第1期69卷 97-102页

作者：王瑞邬绍宸 Roberto F.Weinberg Willia. J.Collins peter a.cawood Sta.e Key La.ora.ory of Geologica. Processes a.d Minera. Resources Institute of Earth SciencesChina University of GeosciencesBeijing 100083China Frontiers Science Center for Deep-time Digita. Ea.th China University of Geosciences(Beijing)Beijing 100083China School of Ea.th Atmosphere and EnvironmentMonash UniversityClayton VIC 3800Australia The Institute for Geoscience Resea.ch Curtin UniversityPerth WA 6102Australia

We a.ply a.zircon redox index to a.globa. compila.ion of detrita. zircons to tra.k the va.ia.ion of oxida.ion sta.e,expressed a.ΔFMQ,through Ea.th's *** from I-type rocks,which comprise ma.tle a.d crusta. igneous protoliths,including tona.ite–trondhjemite–gra.odiorites(TTGs),genera.ly ha.e a.high oxida.ion sta.e(ΔFMQ>0).In contra.t,zircons from igneous rocks derived from supra.rusta. source rocks(S-type)a.e commonly reduced(ΔFMQa.ility density function derived from the Ga.ssia.-Kernel-Density-Estima.ion,we use the ma.imum likelihood estima.ion(MLE)to distinguish Stype from I-type zircons through Ea.th's history using zircon *** S-type ma.ma.production shows a.ca.600 Ma.cyclicity tha. is closely rela.ed to the supercontinent *** link a.cyclic drop in redox va.ues a.ter 2.6 Ga.to periodic S-type ma.ma.genera.ion a.socia.ed with buria. a.d melting of meta.edimenta.y rocks during supercontinent a.sembly a.d ***ΔFMQ of the detrita. zircons rise a.~3.5 Ga.followed by a.consistent a.era.eΔFMQ>0 over the la.t 3 *** tha. the redox sta.e of ma.ma. is independent of crusta. thickness a.d silica.va.ia.ion,a.d eleva.ed va.ues a.e likely more closely rela.ed to tectonic setting,we suggest tha. the consistent a.era.eΔFMQ>0 from ca.3.5 Ga.onwa.ds rela.es to recycling of ocea.ic lithosphere ba.k into the ma.tle in wha. eventua.ly beca.e esta.lished a. subduction *** more reduced ma.ma. a.socia.ed with sedimenta.y sources,beca.e esta.lished a. 2.6 Ga.presuma.ly in response to continenta. rocks rising a.ove sea.evel,a.d follow pea.s of productivity a.socia.ed with the supercontinent cycle.

关键词： Oxida.ion sta.e Supercontinent Wea.hering Subduction Zircon Gra.ite

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

Isotopic a.d geochemica. constra.nts for a.Pa.eoproterozoic a.cretiona.y orogen in the Borborema.Province,NE Bra.il:Implica.ions for reconstructing Nuna.Columbia

引用

Geoscience Frontiers 2022年第5期13卷 267-285页

作者： La.ro Céza. M.de Lira.Sa.tos Geysson a.La.es Fa.rício a.Ca.ito Elton L.Da.ta. peter a.cawood Ha.oldo M.Lima.Felipe Jda.Cruz Lima Depa.ta.ento de Geologia Universidade Federal de PernambucoAv.da ArquiteturaCidade UniversitáriaRecifePEBrazil Serviço Geológico do Bra.il-CPRM Av.SulAfogadosRecifePEBrazil CPMTC Instituto de GeociênciasUniversidade Federal de Minas GeraisAv.Pres.Antônio CarlosPampulhaBelo HorizonteMGBrazil Instituto de Geociência. Universidade de BrasíliaCampus Universitário Darcy RibeiroAsa NorteBrasíliaDFBrazil School of Ea.th Atmosphere and EnvironmentMonash UniversityWellington RdClaytonVIC 3800Australia Depa.ta.ento de Geologia Universidade Federal do CearáCampus do PiciParquelândiaFortalezaCEBrazil

The a.to MoxotóTerra.e of the Borborema.Province presents a.wide exposure of Pa.eoproterozoic crust,but unlike other continenta. blocks of South a.erica.its orogenic history is strongly oblitera.ed by la.e Neoproterozoic *** isotopic a.d geochemica. studies were conducted in ma.ic-ultra.a.ic(Fa.enda.Ca.mo Suite)a.d gra.itic-gneissic rocks(Ria.ho do Na.io Suite)within the *** former present zircon U-Pb crysta.liza.ion a.es a. ca.2.13 Ga.wherea. Sm-Nd da.a.suggests a.juvenile origin via.melting of ea.ly Pa.eoproterozoic to a.chea. peridotitic *** da.a.for these rocks a.e compa.ible with tholeiitic ma.ma. with some degree of crusta. conta.ina.ion a.d tra.e element distribution points to a.continenta.-a.c rela.ed setting interpreted a. remna.ts of the ea.ly sta.es of *** contra.t,the Ria.ho do Na.io Suite wa. empla.ed a. ca.2.08 Ga.a.d ha. highly nega.iveεNd(t)va.ues indica.ing crusta. *** suite displa.s ca.c-a.ka.i to a.ka.i-ca.cic a.d ferroa. geochemica. signa.ures compa.ible with Cordillera. *** a.dition,tra.e-element distribution a. well a. discrimina.t dia.ra.s suggest tha. the precursor ma.ma. were genera.ed during the la.er sta.es of a.continenta. a.c or in a.syn-collisiona. *** on our results,we suggest tha. the studied units might represent missing pieces of a.Pa.eoproterozoic a.cretiona.y orogen tha. formed the crusta. fra.ework of the a.to MoxotóTerra.e,a.d tha. this represents a.block a.socia.ed with a.sembly of the Nuna.Columbia.supercontinent,which is now la.gely hidden within the Neoproterozoic orogenic belts of West Gondwa.a.

关键词： Pa.eoproterozoic a.cretiona.y-collisiona. event Ea.ly orogenic a.d syn-collisiona. ma.ma.ism Pa.eoproterozoic inlier within West Gondwa.a Nuna.Columbia.Supercontinent

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

Genera.ion a.d preserva.ion of continenta. crust in the Grenville Orogeny

引用

Geoscience Frontiers 2015年第3期6卷 357-372页

作者： Christopher J.Spencer peter a.cawood Chris J.Ha.kesworth a.thony R.Pra.e Nick M.W.Roberts Ma.thew S.a.Horstwood Ma.tin J.Whitehouse EIMF Depa.tment of Ea.th a.d Environmenta. Sciences University of St Andrews NERC Isotope Geosciences La.ora.ory British Geological Survey Swedish Museum of Na.ura. History a.d Nordic Center for Ea.th Evolution(NordCEE) Edinburgh Ion Microprobe Fa.ility University of Edinburgh

Detrita. zircons from modern sediments displa. a. episodic tempora. distribution of U-Pb crysta.liza.ion a.es forming a.series of ＇pea.s＇ a.d ＇troughs＇. The pea.s a.e interpreted to represent either periods of enha.ced genera.ion of gra.itic ma.ma.perha.s a.socia.ed with ma.tle overturn a.d superplume events, or preferentia. preserva.ion of continenta. crust during globa. collisiona. orogenesis. The close a.socia.ion of those pea.s with the a.sembly of supercontinents implies a.ca.sa. rela.ionship between collisiona. orogenesis a.d the presence of zircon a.e pea.s. Here these two end-member models （episodic periodicity of increa.ed ma.ma.ism versus selective preserva.ion during collisiona. orogenesis） a.e a.sessed using U-Pb, Hf, a.d 0 a.a.ysis of detrita. zircons from sedimenta.y successions deposited during the - 1.3-1.1 Ga.a.cretiona.y, -1.1-0.9 Ga.collisiona., a.d 〈 0.9 Ga.extensiona. colla.se pha.es of the Grenville orogenic cycle in La.ra.or a.d Scotla.d. The pre-collisiona., a.cretiona.y sta.e provides a.ba.eline of continenta. crust present prior to orogenesis a.d is domina.ed by a.chea. a.d Pa.eoproterozoic a.e pea.s a.socia.ed with pre-1300 Ma.La.rentia. geology. Stra.a.deposited during the Grenville Orogeny displa. simila. a.chea. a.d Pa.eoproterozoic detrita. popula.ions a.ong with a.series of broa. muted pea.s from - 1500 to 1100 Ma. However, post-collisiona. sedimenta.y successions displa. a.domina.t a.e pea. between 1085 a.d 985 Ma. simila. to tha. observed in modern North a.erica. river sediments. Zircons within the post-orogenic sedimenta.y successions ha.e progressively lower EHf a.d higher -lSO va.ues from - 1800 to - 1200 Ma.whereupon they ha.e higher EHf a.d -3180 within the domina.t 1085-985 Ma.a.e pea.. Furthermore, the Lu-Hf isotopic profile of the Grenville-rela.ed a.e pea. is consistent with significa.t a.simila.ion a.d conta.ina.ion by older crusta. ma.eria., The timing of this domina.t a.e pea. coincides with the pea. of meta.orphism a.d

关键词： Zircon Continenta. crust Grenville Orogeny Crusta. preserva.ion

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

青藏高原及其周边前成冰纪综合地层、生物群与古地理演化

引用

中国科学：地球科学 2024年第4期54卷 915-935页

作者：胡培远翟庆国赵国春 peter a.cawood 唐跃刘一鸣中国地质科学院地质研究所北京100037 香港大学地球科学系中国香港999077 大陆动力学国家重点实验室西北大学地质学系西安710069 School of Ea.th Atmosphere&EnvironmentMonash UniversityMelbourneVIC 3800Australia

青藏高原及邻区前成冰纪物质组成及其地质演化过程,在地球早期超大陆形成演化过程的研究中扮演了重要角色.本文系统梳理和总结了青藏高原及邻区前成冰纪沉积岩、古生物、岩浆和变质作用特征.根据现有资料,青藏高原及邻区前成冰纪沉积岩... 详细信息

青藏高原及邻区前成冰纪物质组成及其地质演化过程,在地球早期超大陆形成演化过程的研究中扮演了重要角色.本文系统梳理和总结了青藏高原及邻区前成冰纪沉积岩、古生物、岩浆和变质作用特征.根据现有资料,青藏高原及邻区前成冰纪沉积岩和古生物记录主要集中于中~新元古代,古元古代及更早的记录相对较少,最古老的地质记录为喜马拉雅和昌都地区前寒武纪变质沉积岩中的冥古宙碎屑锆石(约4.0Ga..青藏高原及邻区保存了凯诺兰超级克拉通以及哥伦比亚、罗迪尼亚和冈瓦纳超大陆形成演化过程的记录,其前成冰纪基底可划分为3种类型:塔里木型、扬子型和拉萨型.塔里木型基底与澳大利亚和印度大陆北缘具有古地理亲缘性,且不发育罗迪尼亚超大陆聚合相关的碎屑锆石年龄峰值和岩浆-变质记录(约1.3~0.9Ga.;扬子型基底发育与前成冰纪最晚期全球变冷密切相关的火山活动记录,可见中~新元古代叠层石和微古植物化石,以及约1.1~1.0Ga.罗迪尼亚超大陆聚合相关的岩浆-变质作用记录;拉萨型基底发育新元古代早期大陆裂谷沉积记录(约900Ma.和晚期高压变质事件(约650Ma.,具有明显的1.2~1.1Ga.屑锆石年龄峰值,它很可能与非洲大陆具有古地理亲缘性.

关键词：青藏高原前成冰纪沉积地层古生物群古地理演化

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

欢迎您,

建议与咨询留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

时间限定

文献类型

馆藏选择

核心期刊

语言

文献类型

帮助

文字说明：

检索规则说明：

检索范例：

分类表

所选分类

限定检索结果

文献类型

馆藏范围

日期分布

学科分类号

主题

机构

作者

语言

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

请选择保存的检索档案：

请选择收藏分类：

通借通还

欢迎您,

建议与咨询 留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

时间限定

文献类型

馆藏选择

核心期刊

语言

文献类型

帮助

文字说明：

检索规则说明：

检索范例：

分类表

所选分类

限定检索结果

文献类型

馆藏范围

日期分布

学科分类号

主题

机构

作者

语言

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

请选择保存的检索档案： 新增检索档案 确定 取消

请选择收藏分类： 新增自定义分类 确定 取消

通借通还

建议与咨询留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

请选择保存的检索档案：

请选择收藏分类：