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The Russia.-Ka.a.h a.ta. orogen:a. overview a.d ma.n deba.a.le issues

Geoscience Frontiers 2014年第4期5卷 537-552页

作者： inna Sa.onova Institute of Geology a.d Minera.ogy SB RASKoptyuga Ave.3Novosibirsk 630090Russia Novosibirsk Sta.e University Pirogova St.2Novosibirsk 630090Russia

The pa.er reviews previous a.d recently obta.ned geologica., stra.igra.hic a.d geochronologica. da.a.on the Russia.-Ka.a.h a.ta. orogen, which is loca.ed in the western Centra. a.ia. Orogenic Belt （Ca.B）, between the Ka.a.hsta. a.d Siberia. continenta. blocks. The Russia.-Ka.a.h a.ta. is a.typica. Pa.ific-type orogen, which represents a.colla.e of ocea.ic, a.cretiona.y, fore-a.c, isla.d-a.c a.d continenta. ma.gin terra.es of different a.es sepa.a.ed by strike-slip fa.lts a.d thrusts. Evidence for this comes from key indica.ive rock a.socia.ions, such a. boninite- a.d turbidite （gra.wa.ke）-bea.ing volca.ogenic-sedimenta.y units, a.creted pela.ic chert, ocea.ic isla.ds a.d pla.ea.s, MORB-OIB-protolith blueschists. The three ma.or tectonic doma.ns of the Russia.-Ka.a.h a.ta. a.e：（1） a.ta.-Mongolia. terra.e （a.T）; （2） subduction-a.cretiona.y （Rudny a.ta., Gorny a.ta.） a.d collisiona. （Ka.ba.Na.ym） terra.es; （3） Kura., Cha.ysh-Terekta. North-Ea.t, Irtysh a.d Cha. suture-shea. zones （SSZ）. The evolution of this orogen proceeded in five ma.or sta.es：（i） la.e Neoproterozoic-ea.ly Pa.eozoic subduction-a.cretion in the Pa.eo-a.ia. Ocea.; （ii） Ordovicia.-Siluria. pa.sive ma.gin; （iii） Devonia.-Ca.boniferous a.tive ma.gin a.d collision of a.T with the Siberia. conti- nent; （iv） la.e Pa.eozoic closure of the Pa. a.d coeva. collisiona. ma.ma.ism; （v） Mesozoic post-collisiona. deforma.ion a.d a.a.ogenic ma.ma.ism, which crea.ed the modern structura. colla.e of the Russia.- Ka.a.h a.ta. orogen. The ma.or still unsolved problem of a.ta. geology is origin of the a.ta.-Mongolia. terra.e （continenta. versus a.tive ma.gin）, a.e of a.ta. ba.ement, proportion of juvenile a.d recycled crust a.d origin of the middle Pa.eozoic units of the Gorny a.ta. a.d Rudny a.ta. terra.es.

关键词： a.ta.-Mongolia. terra.eGorny a.d Rudny a.ta. terra.esKa.ba.Na.ymIsla.d a.csPa.eo-a.ia. Ocea.

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Photometric Studies of EV Cnc a.d a. Cnc in the Open Cluster M67

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Resea.ch in a.tronomy a.d a.trophysics 2024年第8期24卷 196-211页

作者： Ma.a.ha.Ra.i G. K.Srira. Deblina.La.iri Vija.a.a. Depa.tment of a.tronomy Osmania UniversityHyderabad 500007India

Conta.t bina.ies a. va.ious sta.es of evolution unveil va.ious opera.ing mecha.isms tha. drive *** report the photometric a.d period va.ia.ion a.a.ysis of two conta.t bina.ies EV Cnc a.d a. Cnc in open cluster *** observed the cluster from the JCBT 1.3 m telescope a.d utilized TESS a.d Kepler *** photometric solutions of EV Cnc a.d a. Cnc revea.ed a.ma.s ra.io of q~0.41 a.d~0.15 with a. inclina.ion of i=42°a.d87°*** solutions suggest tha. EV Cnc is proba.ly a.semi-deta.hed a.d a. Cnc is a.deep low-ma.s ra.io conta.t *** study of O-C va.ia.ion a.a.ysis indica.es tha. for both systems,the period is increa.ing which suggests the ma.s tra.sfer is occurring from seconda.y to *** the ca.e of a. Cnc a.d ba.ed on simula.ions by ra.domly va.ying the time of minima.to fit the LITE solution,we noted the third body orbita. period to be a.ound P_(3)=26.82±2.54 yr,which is different from ea.lier reported va.ues a.d conclude tha. future observa.ions a.e required to confirm this *** compa.e these two systems with other simila. conta.t bina.ies to get a. estima.e of the fina. configura.ion of the respective systems.

关键词： (sta.s)bina.ies(including multiple) close-(sta.s)bina.ies eclipsing-sta.s a.tivity

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Kerogen Kinetic Distributions a.d Simula.ions Provide Insights into Petroleum Tra.sforma.ion Fra.tion (TF) Profiles of Orga.ic-Rich Sha.es

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Journa. of Ea.th Science 2024年第3期35卷 747-757页

作者： Da.id a.Wood DWa.Energy Limited Lincoln LN59JPUnited Kingdom

Two hundred a.d fifty single first-order a.rhenius rea.tions a.e simula.ed to genera.e S2 pyrogra.s a. three hea.ing ra.es 25,15,a.d 5°C·*** a.tiva.ion energy(E)a.d pre-exponentia. fa.tor(a.of the rea.tions simula.ed follow a.long-esta.lished trend of those va.ia.le va.ues displa.ed by sha.es a.d *** cha.a.teristics of the tra.sforma.ion fra.tion(TF)profiles(product genera.ion window tempera.ures)of the simula.ed single rea.tions a.e compa.ed to the TF profiles of recorded sha.e pyrogra.s genera.ed by multiple rea.tions with different E-a.va.ues lying nea. the defined E-a.*** simila.ities a.d differences a.e observed between the TF profile va.ues of the two *** simila.ities support the sprea. of E-a.va.ues involved in sha.e pyrogra. best *** differences a.e most likely expla.ned by the complexity of the multiple kerogen first-order a.d second-order rea.tions contributing to the recorded sha.e pyrogra.s versus the simplicity a.d crispness of the single first-order rea.tions *** results a.so justify the va.idity of using the previously described“va.ia.le E-a.pyrogra.-fitting method”of multi-hea.ing-ra.e sha.e pyrogra.s ena.ling optimizers to choose multiple rea.tions from a. unlimited ra.ge of E-a.*** contra.t,further doubt is ca.t on the va.idity of the consta.t-a.pyrogra.-fitting method used by the Ea.y%Ro technique,in tha. a.distribution of rea.tions with a.single a.va.ue is unlikely to represent the complex va.iety of kerogen ma.era.s observed in sha.e *** profiles genera.ed by the va.ia.le E-a.pyrogra.-fitting method lie close to the esta.lished E-a.trend a.d a.e likely to provide more rea.istic TF genera.ion window tempera.ures tha. TF profiles genera.ed by the consta.t-a.pyrogra.-fitting method.

关键词： tra.sforma.ion fra.tion profiles simula.ed S2 pyrogra.s multiple hea.ing ra.es kerogen/sha.e kinetics S2 pyrogra. fitting techniques kerogen petroleum resea.ch.

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Ophiolites of the Centra. a.ia. Orogenic Belt:Geochemica. a.d petrologica. cha.a.teriza.ion a.d tectonic settings

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Geoscience Frontiers 2019年第4期10卷 1255-1284页

作者： Ha.a.d Furnes inna Sa.onova Depa.tment of Ea.th Science University of BergenAllegt.415007BergenNorway Sobolev Institute of Geology a.d Minera.ogy 3 Koptyuga ave.Novosibirsk 630090Russia Novosibirsk Sta.e University 1Pirogova St.Novosibirsk 630090Russia

We present a.compila.ion of published da.a.field,petrogra.hy,a.es a.d geochemistry)from 73 ophiolitic complexes of the Centra. a.ia. Orogenic *** ophiolitic complexes,ra.ging in a.e from Neoproterozoic to *** been geochemica.ly cla.sified a. subduction-rela.ed a.d subductionunrela.ed ca.egories a.plying recent,well-esta.lished discrimina.ion *** subductionunrela.ed ca.egory is further subdivided into Mid-Ocea. Ridge type(MOR),a.common rift-drift sta.e a.d Plume type,a.d the subduction-rela.ed ca.egory is subdivided into Ba.ka.c(Ba.,Forea.c(Fa..Ba.ka.c to Forea.c(Ba.Fa.a.d Volca.ic a.c(Va.*** four subduction-rela.ed types define highly different geochemica. fea.ures,with the Ba.a.d Fa.types defining end members showing subduction influence of 10%-100%a.d 90%-100%subduction influence,respectively,a.d the two other types(Ba.a.a.d Va.define va.ues between the two end *** subduction-rela.ed ca.egory comprises79%of the exa.ined ophiolites,of which the Ba.type ophiolites is by fa. the domina.t group,followed by the Ba.Fa.type,a.d with Fa.a.d Va.types a. subordina.e *** Neoproterozoic a.d Ordovicia. complexes exhibit the highest,wherea. those of Siluria. a.e exhibit the lowest *** the rema.ning 21%subduction-unrela.ed ophiolites,the MOR type *** the subductionrela.ed a.d subduction-unrela.ed types,in pa.ticula. the la.ter,a.e commonly a.socia.ed with a.ka.ine ba.a.ts ta.en to represent ocea. isla.d ***,dunite,ga.bro a.d ba.a.t a.e the common lithologies in a.l ophiolite types,wherea. the Ba.Fa.Fa.a.d Va.types genera.ly conta.n intermedia.e to felsic rocks,a.d in the Fa.type boninites *** subduction-rela.ed ophiolites types genera.ly show low meta.orphic gra.e,wherea. *** a.d blueschist gra.es occur in the subduction-unrela.ed a.d Ba.*** highly different subduction contribution(from 0 to 100%in the MOR a.d Fa.respectively),a.test to va.ia.le dips of t

关键词： Geochemica. cla.sifica.ion Subduction-unrela.ed units Subduction-rela.ed units Subduction fingerprint Intra.pla.e ma.ma. a.c erosion

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Synthesis of hiera.chica. mesoporous Ln_(2)Ti_(2)O_(7)(Ln=Y,Tb-Yb)pyrochlores a.d ura.yl sorption properties

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Journa. of Ma.eria.s Science & Technology 2022年第18期113卷 22-32页

作者： Linggen Kong inna Ka.a.chevtseva.Ta. Wei Nichola. Sca.es a.stra.ia. Nuclea. Science a.d Technology Orga.isa.ion Lucas Heights NSW2234Australia

Mesoporous structured meta. oxides exhibit ma.y a.tive ***,the synthesis of crysta.line meta. oxides with a.terna.y composition while ma.nta.ning sa.isfa.tory pore fea.ures is ***,high tempera.ures a.e required which inhibit control of pore structure properties including surfa.e a.ea.pore volume,a.d pore ***,the synthesis of terna.y meta. oxides Ln_(2)Ti_(2)O_(7)pos-sessing pyrochlore crysta. structure is a.hieved using a.novel technique which combines‘soft’a.d ha.d colloid templa.ing *** formed ma.eria.s a.e of submicron size a.d composed of∼25-30 nm product‘building blocks’with good chemica. a.d pha.e *** polycrysta.line powders ha.e a.high specific surfa.e a.ea.up to 70 m^(2)·g^(-1))a.d pore volume(∼0.35 cm^(3)·g^(-1))which result in a.good a.sorp-tion ca.a.ity(U upta.e closing to 60 mg·g^(-1)).Rema.ka.ly,the ma.eria. exhibits a.significa.t portion of mesopores(ma.nly 10-40 nm)which fa.ilita.e fa.t a.sorption of the ca.ions due to high *** synthetic methodology described herein produces highly homogenous powders a.d ca. be a.plied to other compositions a.d structures.

关键词： Porous terna.y meta. oxides Dua. templa.e synthesis La.tha.ide tita.a.e Pyrochlore Ura.ium a.sorption

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Mud volca.o origin of the Mottled Zone,South Leva.t

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Geoscience Frontiers 2013年第5期4卷 597-619页

作者： Igor Novikov Yevgeny Va.nik inna Sa.onova Institute of Geology a.d Minera.ogy SB Ra. Koptuyga Ave.3Novosibirsk 630090Russia Depa.tment of Geologica. a.d Environmenta. Sciences Ben-Gurion University of the NegevP.O.B.653Beer-Sheva 84105Israel

The Mottled Zone（MZ） or Ha.rurim Forma.ion,which occurs nea. the Leva.tine Tra.sform in the South Leva.t,ha. been studied during the la.t 150 yea.s but its origin rema.ns *** Zone Complex/Complexes（MZC/MZCs） consist of breccia.ed ca.bona.e a.d low-tempera.ure ca.cium-hydro-silica.e rocks,which include unusua. high- a.d ultra.high-tempera.ure low-pressure（HT-LP） meta.morphic minera. *** MZ ha. been rega.ded a. a.product of combustion of bituminous cha.ks of the Gha.eb *** Creta.eous（Ma.strichtia.） *** this pa.er we present deta.led geogra.hic, geomorphologic,structura. a.d geologica. da.a.from the MZCs of the South Leva.t,which show tha. the MZCs ca.not be stra.igra.hica.ly correla.ed with the Gha.eb Fm.,beca.se MZC la.e Oligocene-la.e Pleistocene deposits occur within or unconforma.le i.e.,with stra.igra.hic hia.us,overla. both the la.e Creta.eous a.d,in pla.es,Neogene stra.igra.hic *** propose a. a.terna.ive model for the forma.ion of MZCs by tectonica.ly induced mud volca.ism during la.e Oligocene-la.e Pleistocene time. This model expla.ns（i） the presence of dikes a.d tube-like bodies,which consist of breccia.ed exotic cla.tic ma.eria. derived from stra.igra.hica.ly a.d hypsometrica.ly lower horizons;（ii） minera. a.sembla.es of sa.idinite fa.ies meta.orphism;（iii） multi-sta.e cha.a.ter of HT-LP pyrometa.orphism;a.d （iv） multi-sta.e low-tempera.ure hydrotherma. *** tempera.ures（up to 1500℃） minera. a.sembla.es resulted from combustion of hydroca.bon ga.es of mud *** volca.ism wa. spa.ia.ly a.d structura.ly rela.ed to neotectonic folds a.d deforma.ion zones formed in response to opening of the Red Sea.rift a.d propa.a.ion of the Leva.tine Tra.sform *** model ma. significa.tly cha.ge the prospects for oil-a.d-ga. deposits in the region.

关键词： HT-LP sa.idinite fa.ies meta.orphism Geomorphology Dea. Sea Leva.tine Tra.sform Neotectonics Hydroca.bon tra.s

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Optimiza.ion Problem for the Integra. Model of Developing Systems

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Journa. of the Opera.ions Resea.ch Society of China 2022年第4期10卷 817-833页

作者： Evgeniia.Ma.kova.inna Sidler Victor Trufa.ov Melentiev Energy Systems Institute of Siberia. Bra.ch of the Russia. a.a.emy of Sciences Irkutsk664033Russia

This pa.er a.dresses a. integra. model of development a.la.ge electric power system using the exa.ple of the Unified Energy System of *** model ta.es a.count of the a.e structure of the pla.ts ma.n ***,genera.ing equipment is divided into components depending on the types of energy resources *** ma.hema.ica. model is presented by a.system of noncla.sica. Volterra.integra. equa.ions of the first *** of the equa.ions describes the ba.a.ce between the tota. a.a.la.le ca.a.ity of the electric power system,commissioning of new equipment,a.d disma.tling of obsolete *** other equa.ions define the sha.es of different types of power pla.ts in the tota. composition of the electric power system *** on the considered model,we set a.problem tha. sea.ches the optima. lifetimes of electric power system ca.a.ities for a.given dema.d for *** optima.ity criterion is a.functiona. reflecting cost of commissioning a.d opera.ing the *** specifics of the optimiza.ion problem a.e tha. the optimiza.ion pa.a.eter is in the lower limit of *** a.gorithm for solving of this optima. control problem numerica.ly is *** influence of economic indices on the solution to the optima. control problem is *** of the optima. development of the Unified Energy System of Russia.until 2050 a.e ca.ried out using rea.-life da.a.

关键词： Optimiza.ion problem Integra. model Lifetime

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Triggers a.d sources of vola.ile-bea.ing plumes in the ma.tle tra.sition zone

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Geoscience Frontiers 2015年第5期6卷 679-685页

作者： inna Sa.onova.Konsta.tin Lita.ov Shigenori Ma.uya.a V.S.Sobolev Institute of Geology a.d Minera.ogy SB Ra. Novosibirsk Sta.e University Ea.th-Life Science Institute Tokyo Institute of Technology

The pa.er discusses genera.ion of vola.ile-bea.ing plumes in the ma.tle tra.sition zone(MTZ) in terms of minera.-fluid petrology a.d their rela.ed forma.ion of numerous loca.ities of intra.pla.e bimoda. volca.ic series in Centra. a.d Ea.t *** plume genera.ion in the MTZ ca. be triggered by the tectonic erosion of continenta. crust a. Pa.ific-type convergent ma.gins a.d by the presence of wa.er a.d ca.bon dioxide in the *** proba.le sources of vola.iles a.e the hyclra.ed/ca.bona.ed sediments a.d ba.a.ts a.d serpentinite of ocea.ic sla.s,which ca. be subducted down to the deep *** erosion of continenta. crust supplies crusta. ma.eria. enriched in ura.ium a.d thorium into the ma.tle,which ca. serve source of hea. in the *** hea.ing in the MTZ induces melting of subducted sla.s a.d continenta. crust a.d ma.tle upwelling,to produce OIB-type ma.ic a.d felsic melts,respectively.

关键词： a.is Pa.ific-type convergent ma.gin Continenta. cr

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Rodent biology a.d ecologica.ly ba.ed rodent ma.a.ement(EBRM)-25 yea.s of progress through promoting multidisciplina.y resea.ch

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Integra.ive Zoology 2024年第1期19卷 2-7页

作者： Gra.t R. SINGLETON Lyn a. HINDS Rhodes Ma.UNDI Steven R. BELMa.N Na.ura. Resources Institute University of Greenwich Kent UK CSIRO Hea.th a.d Biosecurity Canberra ACT Australia a.rica. Centre of Excellence for Innova.ive Rodent Pest Ma.a.ement a.d Biosensor Technology Development Sokoine University of Agriculture Morogoro Tanzania Institute of Pest Ma.a.ement Sokoine University of Agriculture Morogoro Tanzania

“During rodent outbrea. yea.s in ea.tern a.rica.lo-ca.ly,more tha. 80%of the potentia. ha.vest ma. be lost,but even in non-outbrea. periods,rodents ca.se chronic da.a.e to crops….The pest rodent story in a.rica.in-volves severa. species embedded in a.broa. a.d va.ia.le la.dsca.e with highly va.ia.le densities.”(Leirs et a..2010).

关键词： da.a.e crops

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Inhibition of CXCR4/CXCL12 signa.ing:a.tra.sla.iona. perspective for a.zheimer’s disea.e trea.ment

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Neura. Regenera.ion Resea.ch 2022年第1期17卷 108-109页

作者： Yuva. Ga.riel inna Ra.inovich-Nikitin Beka.Solomon The Shmunis School of Biomedicine a.d Ca.cer Resea.ch George S.Wise Faculty of Life SciencesTel Aviv UniversityTel AvivIsrael

The mecha.ism of a. rema.ns uncovered:The current ma.nstrea. doctrine in a.zheimer’s disea.e(a.)is the a.yloid ca.ca.e *** to this hypothesis,a.yloid-β(a.)deposition is the ma.n rea.on for neurofibrilla.y ta.gles f... 详细信息

关键词： a.zheimer a.yloid a.

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