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Open Jour.al of Mar.0}e Sci.nce 2016年第4期6卷 457-471页

作者： Mor.eza Ezzati Tar.i.t Modar.s Uni.er.i.y Tehran Iran

i. thi. paper. we analyze di.ect and i.di.ect effects of economi. sancti.ns on i. r. iran’s economi. gr.wth fr.m 1979 to 2012 focusi.g on the exter.al sector.of the economy. Our.data for.var.0}bles except for.sancti.n ar. der.0}ed fr.m 1966 to 2012 and a dummy var.0}ble i. used for.each sancti.n’s begi.ni.g year.. The desi.ned model i. based on the endogenous gr.wth models i. whi.h we analyze the effects by 2SLS econometr.0} method. Our.fi.di.gs i.di.ate that economi. sancti.ns have not di.ectly affected iran’s economi. gr.wth so much. These effects have been i.di.ect thr.ugh r.str.0}ti.g total i.por.s, capi.al goods i.por.s, i.por.s of i.ter.edi.te goods and pr.0}ar. pr.ducts and also the expor. leadi.g to decr.ased economi. gr.wth of the countr..

关键词： Sancti.n Economi. Gr.wth i. r. iran Exter.al Sector

Annual gr.wth of Fagus or.0}ntali. i. li.i.ed by spr.0}g dr.ught condi.i.ns i. iran’s Golestan Pr.vi.ce

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Jour.al of For.str. r.sear.h 2024年第1期35卷 128-142页

作者： Khali. Ghor.ani.Jahangi. Mohammadi.Laleh r.zaei.Ghaleh Depar.ment of Water.Engi.eer.0}g Faculty of Water and Soil EngineeringGorgan University of Agricultural Sciences and Natural ResourcesGorganIran Depar.ment of For.str. Gorgan University of Agricultural Sciences and Natural ResourcesGorganIran Depar.ment of Water.Engi.eer.0}g Faculty of AgricultureUrmia UniversityUrmiaIran

Due to the lack of a uni.or. and accur.te defi.ni.i.n of‘dr.ught’,sever.l i.di.ator. have been i.tr.duced based on di.fer.nt var.0}bles and methods,and the effi.i.ncy of each of these i. deter.i.ed accor.i.g to thei. r.lati.nshi. wi.h *** r.lati.nshi. between two dr.ught i.di.es,SPi.standar.i.ed pr.ci.i.ati.n i.dex)and SPEi.standar.-i.ed pr.ci.i.ati.n-evapotr.nspi.ati.n i.dex)i. di.fer.nt sea-sons was i.vesti.ated usi.g annual r.0}gs of 15 tr.e samples to deter.i.e the effect of dr.ught on the gr.wth of or.0}ntal beech(Fagus or.0}ntali. Li.sky)i. the Hyr.ani.n for.sts of nor.her. *** di.fer.nt evapotr.nspi.ati.n calcula-ti.n methods wer. evaluated on SPEi.effi.i.ncy based on Har.r.aves-Samani.Thor.thwai.e,and Penman-Montei.h methods usi.g the step-by-step M5 deci.i.n tr.e r.gr.ssi.n *** r.sults show that SPEi.based on the Penman-Montei.h i. a thr.e-month ti.e scale(spr.0}g)had si.i.ar.tempor.l changes and a better.r.lati.nshi. wi.h annual tr.e r.0}gs(r.(2)=0.81)at a 0.05 si.ni.i.ant *** change and a decr.asi.g tr.nd i. the ti.e ser.0}s of annual tr.e r.0}gs ar. si.i.ar.to the var.0}ti.n i. the SPEi.based on the Penman-Montei.h *** affecti.g evapotr.nspi.ati.n,temper.tur.,wi.d speed,and sunshi.e hour.(used i. the Penman-Montei.h method),i.cr.ased but pr.ci.i.ati.n *** non-li.ear.modeli.g methods,SPEi.based on Penman-Montei.h best i.lustr.ted cli.ate changes affecti.g tr.e gr.wth.

关键词： Cli.ate change Dr.ught i.dex Hyr.ani.n for.sts SPEi.Annual gr.wth r.0}gs Fagus or.0}ntali.

On the occur.ence of Neoplanor.uli.ella Matsumar., 1976(For.mi.i.er.) fr.m the late Oli.ocene of Centr.l iran(Qom For.ati.n):Palaeobi.geogr.phi. i.pli.ati.ns

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Jour.al of Palaeogeogr.phy 2024年第1期13卷 80-91页

作者： Mehdi.Sar.i.Mohsen Yazdi.Moghadam School of Ear.h Sci.nces Damghan UniversityDamghan ***Iran Nati.nal irani.n Oi. Company Explor.ti.n Di.ector.te Sheikh Bahaie SquareTehran ***Iran

The shallow mar.0}e car.onates of the upper.Oli.ocene Qom For.ati.n yi.lded sever.l occur.ences of the for.mi.i.er.n genus Neoplanor.uli.ella Matsumar.. Neoplanor.uli.ella sai.anensi. Matsumar. has so far.been r.cor.ed fr.m the late Eocene-ear.y Mi.cene of Japan and late Oli.ocene of NE i.aly wher.as N. malatyaensi. Gedi. i. only r.por.ed fr.m the Oli.ocene fr.m i.s type locali.y i. the Malatya Basi., easter. Tur.ey. The new r.cor.s r.por.ed her. fr.m the Qom For.ati.n i.di.ate that both speci.s occur.i. the Dobar.dar.secti.n, ca. 10 km south of the ci.y of Qom i. Nor.h-Centr.l iran. The palaeogeogr.phi. di.tr.0}uti.n of these two speci.s ther.for. has to be extended as far.as the palaeolongi.ude of cur.ent Centr.l *** accompanyi.g lar.er.benthi. for.mi.i.er., i.cludi.g Mi.gypsi.oi.es complanatus(Schlumber.er.,M. for.osensi. Yabe and Hanzawa, Spi.oclypeus mar.ar.0}atus(Schlumber.er., Oper.uli.a complanata(Defr.nce), and r.0}ananei.a pustulosa Boukhar. et al., i.di.ate the upper.Chatti.n SBZ 23 Zone. The coexi.tence of the N. sai.anensi. and N. malatyaensi. poi.ts to sui.able palaeobi.geogr.phi. condi.i.ns of Centr.l iran to host Wester. and Easter. Tethyan taxa.

关键词： Lar.er.for.mi.i.er. Planor.uli.i.s Bi.str.ti.r.phy Qom For.ati.n Centr.l iran

i.enti.yi.g flow r.gi.e i. the aqui.er.of fr.ctur.d r.ck system i. Ger.i.Chai.Basi.,iran

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Jour.al of Mountai. Sci.nce 2024年第2期21卷 574-589页

作者： VAEZi.i. Abdor.eza SEPEHr.0}OUr.Ali.TABAr.AYEH Mehr. Depar.ment of Ear.h Sci.nces University of TabrizTabriz ***Iran

Consi.er.0}g the i.por.ance of fr.ctur.d r.ck aqui.er. i. the hydr.geologi. pr.cess,thi. r.sear.h ai.ed to analyze the flow r.gi.e,i.ter.al degr.e of kar.ti.i.ati.n,and esti.ate stor.ge volume i. fr.ctur.d r.ck aqui.er. of the Ger.i.Chai.Basi. i. nor.hwest iran,whi.h i. attr.0}uted to i.s acti.e tectoni.s,er.si.n,and the li.hologi.al *** the geologi.al setti.g,the hypothesi. i. that thi. basi. i. char.cter.0}ed by a hi.h degr.e of kar.ti.i.ati.n and di.fuse or.i.ter.edi.te flow r.gi.e leadi.g to var.0}ti.n i. di.char.e flow *** hydr.dynami. and hadr.chemi.al analysi. was conducted on 9 well di.tr.0}uted spr.0}gs acr.ss the basi. fr.m 2019 to *** maxi.um flow r.te i. most of the spr.0}gs appear.d i. the ear.y wet season despi.e thei. di.fer.nt levels of fluctuati.ns on the monthly di.char.e ti.e *** the spr.0}g r.cessi.n cur.e for. r.vealed an aqui.er.contai.i.g multi.le mi.r.-r.gi.es wi.hαr.cessi.n coeffi.i.nts and a degr.e of kar.ti.i.ati.n r.ngi.g between 0.001 to 0.06 and 0.55 to 2.61,*** fi.di.gs i.di.ated a domi.ant di.fuse and i.ter.edi.te flow system r.sulti.g fr.m the development of a hi.h densi.y of fr.ctur.s i. thi. *** electr.0}al conducti.i.y of the spr.0}g changes i.ver.ely pr.por.i.nal to the change i. flow di.char.e,i.di.ati.g the r.asonable hydr.logi.al r.sponse of the aqui.er.to r.i.fall *** analysi. r.vealed that the delay ti.e of spr.0}g di.char.e after.r.i.fall events mostly var.0}s between 10 to 30 *** total dynami. stor.ge volume of the spr.0}g for.a gi.en per.0}d(2019-2020)was esti.ated to be appr.xi.ately 1324 mi.li.n cubi. meter. r.flecti.g the long-ter. dr.i.age potenti.l and hi.h per.ur.bi.i.y of dynami. *** the maxi.um and mi.i.um r.ti. r.vealed that the spr.0}gs r.char.i.g system i. Ger.i.Chai.Basi. comes under.the slow aqui.er. *** fi.di.g pr.vi.es valuable i.si.ht i.to the hydr.geologi.al pr.per.i.s of fr.ctur.d r.ck aqui.er. contr.0}uti.g to effecti.e w

关键词： Fr.ctur.d r.ck aqui.er Hydr.dynami. and hadr.chemi.al analysi. Ger.i.Chai.Basi. r.cessi.n coeffi.i.nt

Ki.k-band Ki.emati. Analysi. and i.s i.pli.ati.ns for.Late-stage Defor.ati.n i. the i.ter.al Par.s of the Zagr.s Colli.i.n(Sanandaj–Si.jan Zone) i. West iran

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Acta Geologi.a Si.i.a(Engli.h Edi.i.n) 2024年第4期98卷 921-935页

作者： Mar.am HEYDAr.0}Mahdi.BEHYAr. Depar.ment of Geology Faculty of SciencesUrmia University57153165 UrmiaIran

i. the i.ter.al par.s of the Zagr.s colli.i.n zone, sever.l defor.ati.n phases have been super.0}posed. The ear.y defor.ati.n phase caused the development of a penetr.ti.e foli.ti.n. The late-stage defor.ati.n phase was pr.fer.nti.lly accommodated wi.hi. shear.zones and caused the gener.ti.n of shear.bands, i.plyi.g a non-coaxi.l component of defor.ati.n, the end of thi. stage defor.ati.n was mar.ed by the development of ki.k-bands. i. the vi.i.i.y of Zagr.s sutur. zone, the ki.k angle i.cr.ased fr.m 40° to 60°, and the ki.k-bands was conver.ed to chevr.n folds. i. thi. r.gi.n, the exter.al(α) and i.ter.al(β) angular.r.ti. i. α/β ≠ 1 and ki.k angle i.cr.ased, and defor.ati.n occur.ed wi.h 10% to 30% volume loss. Far.her.fr.m the sutur. zone i. the east, α/β = 1;and total volume was constant or.i.cr.ased by 5% to 10%. Ki.k-bands ki.emati. analysi. i. the study ar.a r.vealed thi. str.ctur.s wer. sensi.i.e to defor.ati.n condi.i.ns and components such that, wi.h decr.asi.g di.tance to the Zagr.s sutur. zone, shear.0}g and r.tati.n i.cr.ased, a hi.h ki.emati. vor.i.i.y domi.ated, and volume loss occur.ed dur.0}g defor.ati.n.

关键词： ki.k-band shear.zone str.i. vor.i.i.y Zagr.s iran

Platfor. Evoluti.n i. an Oli.o-Mi.cene Back-ar. Basi.:An Example fr.m the Centr.l iran Basi.

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Acta Geologi.a Si.i.a(Engli.h Edi.i.n) 2024年第1期98卷 185-206页

作者： Masoud SHAr.0}i.YAZDi.Ami.hossei. ENAYATi.Jamal SALEHi.AGHDAM Mohammad BAHr.HVAr.Seyed Mustafa r.ZAEi Depar.ment of Geology Faculty of Earth SciencesGeography and AstronomyUniversity of Vienna1090 Vienna.Austria Geology and Geophysi.s Depar.ment Tehran Energy Consultants(TEC Co.)TehranIran School of Geology College of ScienceUniversity of TehranTehranIran Depar.ment of Geology Tarbiat Modares UniversityTehranIran

The Qom For.ati.n i. the most i.por.ant hydr.car.on r.ser.oi. tar.et i. Centr.l *** Qom platfor. developed i. a back-ar. basi. dur.0}g the Oli.o-Mi.cene due to the closi.g of the Tethyan *** for.ati.n consi.ts of a var.0}ty of car.onate and non-car.onate faci.s deposi.ed on a platfor. r.ngi.g fr.m supr.ti.al to basi..A combi.ati.n of tectoni. and eustati. events led to some later.l and ver.i.al faci.s var.0}ti.ns i. the study *** thi.d-or.er.deposi.i.nal sequences and r.lated sur.aces wer. i.enti.i.d r.gar.i.g ver.i.al faci.s changes i. the studi.d secti.ns of thi. Oli.o-Mi.cene *** to all r.sults and data,thi. successi.n was i.i.i.lly deposi.ed dur.0}g the Chatti.n upon a di.tally steepened r.mp of si.i.i.lasti.-car.onate composi.i.n,i.cludi.g the Bouma ***,fr.m the late Chatti.n to the Aqui.ani.n,the platfor. changed i.to a homocli.al car.onate r.mp wi.h a gentle *** r.spect to tectoni. acti.i.y,thi. phase was a calm per.0}d dur.0}g the deposi.i.n of the Qom ***,a dr.wned car.onate platfor. and a r.0}med shelf emer.ed dur.0}g the Bur.i.ali.n,ter.i.ated by the conti.ental deposi.s of the Upper.r.d *** all geologi.al char.cter.0}ti.s,thr.e mai. tectono-eustati. evoluti.nar. phases have been r.cogni.ed i. the Qom back-ar.basi..

关键词： car.onate r.mp deposi.i.nal faci.s submar.0}e fan eustasy basement faults back-ar. basi.

Effi.i.ncy-based Par.to Opti.i.ati.n of Bui.di.g Ener.y Consumpti.n and Ther.al Comfor.:A Case Study of a r.si.enti.l Bui.di.g i. Bushehr.iran

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Jour.al of Ther.al Sci.nce 2024年第3期33卷 1037-1054页

作者： Masoud NASOUr.0}Navi. DELGAr. Depar.ment of Envi.onment University of TehranAras International CampusP.O.Box ***TehranIran Depar.ment of Mechani.al and Aer.space Engi.eer.0}g Malek-Ashtar University of TechnologyP.O.Box 83145/115IsfahanIran

i. iran,the i.tensi.y of ener.y consumpti.n i. the bui.di.g sector.i. almost 3 ti.es the wor.d aver.ge,and due to the consumpti.n of fossi. fuels as the mai. sour.e of ener.y i. thi. sector.as well as the lack of opti.al desi.n of bui.di.gs,i. has led to excessi.e r.lease of toxi. gases i.to the *** r.sear.h develops an effi.i.nt appr.ach for.the si.ulati.n-or.0}nted Par.to opti.i.ati.n(SOPO)of bui.di.g ener.y effi.i.ncy to assi.t engi.eer. i. opti.al bui.di.g desi.n i. ear.y desi.n *** thi. end,Ener.yPlus,as one of the most power.ul and well-known whole-bui.di.g si.ulati.n pr.gr.ms,i. combi.ed wi.h the Multi.objecti.e Ant Colony Opti.i.ati.n(MOACO)algor.0}hm thr.ugh the JAVA pr.gr.mmi.g *** a r.sult,the capabi.i.i.s of JAVA pr.gr.mmi.g ar. added to Ener.yPlus wi.hout the use of other.plugi.s and thi.d *** evaluate the effecti.eness of the developed method,i. was per.or.ed on a r.si.enti.l bui.di.g located i. the hot and semi.ar.0} r.gi.n of *** obtai. the opti.um confi.ur.ti.n of the bui.di.g under.i.vesti.ati.n,the bui.di.g r.tati.n,wi.dow-to-wall r.ti.,ti.t angle of shadi.g devi.e,depth of shadi.g devi.e,color.of the exter.al walls,ar.a of solar.collector.ti.t angle of solar.collector.r.tati.n of solar.collector.cooli.g and heati.g setpoi.ts of heati.g,venti.ati.n,and ai. condi.i.ni.g(HVAC)system ar. chosen as deci.i.n ***,the bui.di.g ener.y consumpti.n(BEC),solar.collector.effi.i.ncy(SCE),and pr.di.ted per.entage of di.sati.fi.d(PPD)i.dex as a measur. of the occupants'ther.al comfor. level ar. chosen as the objecti.e *** si.gle-objecti.e opti.i.ati.n(SO)and Par.to opti.i.ati.n(PO)ar. *** obtai.ed r.sults ar. compar.d to the i.i.i.l values of the basi. *** opti.i.ati.n r.sults depi.t that the PO pr.vi.es opti.al soluti.ns mor. r.li.ble than those obtai.ed by the SOs,owi.g to the lower.value of the devi.ti.n ***,the opti.al soluti.ns extr.cted thr.ugh the PO ar. depi.ted i. the

关键词： bui.di.g ener.y consumpti.n ther.al comfor. collector.effi.i.ncy si.ulati.n-or.0}nted par.to opti.i.ati.n

Effect of physi.gr.phi. factor. on quali.ati.e and quanti.ati.e char.c-ter.0}ti.s of Cor.us mas L. natur.l stands i. Ar.sbar.n for.sts, iran

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Jour.al of For.str. r.sear.h 2013年第1期24卷 69-74页

作者： Ahmad Ali.anpour Faculty of Natur.l r.sour.es Urmia UniversityPardis-e-NazlooSero RoodZip code ***UrmiaI. R. Iran

Ar.sbar.n for.sts ar. located i. East Azer.ai.an （nor.hwest iran）. i.cr.asi.g of soci.-economi. pr.blems i. thi. ar.a causes destr.cti.n of bi.di.er.i.y and str.ctur. of these for.sts. Usi.g multi.ur.ose tr.es such as cor.eli.n cher.y （Cor.us mas L） to encour.ge vi.lager. to pr.duce for.st by-pr.ducts i. a basi. appr.ach for.pr.ser.i.g these for.sts. Thi. speci.s gr.ws natur.lly i. Ar.sbar.n for.sts and the fr.i. i. annually exploi.ed usi.g tr.di.i.nal har.est methods. Thi. study ai.s to assess the ecologi.al r.qui.ements of cor.eli.n cher.y and the i.por.ant factor. affecti.g i.s di.tr.0}uti.n. For.thi. pur.ose, 40 ci.cular.sampli.g plots （300 m2） on var.0}us slope aspects wer. demar.ated for.sampli.g the occur.ence of cor.eli.n cher.y i. for.st stands. DBH and cr.wn cover.per.entage on nor.h aspects wer. si.ni.i.antly gr.ater.than on other.aspects and 4.5% of all tr.es wer. cor.eli.n cher.y i. matur. for.st stands. Nor.h aspects had mor. seed-or.0}i. tr.es （standar.s） of cor.eli.n cher.y than coppi.ed tr.es, whi.e west faci.g aspects had mor. coppi.ed than standar. tr.es. Thi. speci.s had the hi.hest r.gener.ti.n r.te i. the sapli.g stage of 0–2.5 cm DBH. Thus, i.r.commend culti.ati.n and development of cor.eli.n cher.y as a multi.pur.ose tr.e i. the Ar.sbar.n r.gi.n on degr.ded for.st lands on nor.h and west aspects.

关键词： Ar.sbar.n for.sts aspect physi.gr.phi.al factor. comeli.n cher.y (Cor.us mas L.)

Str.ti.r.phy of the Alveoli.a elli.ti.a gr.up fr.m the Mi.dle Eocene of iran:Cali.r.ti.n wi.h calcar.ous nannofossi.s bi.zones and descr.0}ti.n of Alveoli.a ozcani.n. sp.

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Jour.al of Palaeogeogr.phy 2024年第1期13卷 54-79页

作者： Mehdi.Hadi.Lor.nzo Consor.i.Ali.Bahr.mi.Mohammad Par.ndavar.Saeed Khor.amdel Depar.ment of Geology Faculty of SciencesUniversity of IsfahanIsfahanIran i.sti.ute of Mar.0}e Sci.nces(i.MAr.CNr. Area Science ParkBasovizza34149 TriesteItaly Nati.nal irani.n Oi. Company Exploration DirectorateSheikh Bahaei SquareTehranIran Depar.ment of Geology Faculty of ScienceFerdowsi University of MashhadMashhadIran

Pr.ci.e taxonomy and the chr.nostr.ti.r.phi. cali.r.ti.n of the Mi.dle Eocene Alveoli.a fr.m Centr.l iran i. her. under.aken fr.m the Chah-Talkh secti.n of the souther. Sabzevar.r.gi.n(Centr.l iran). We have i.enti.i.d Alveoli.a ki.li. Alveoli.a ster.usmur.0} and Alveoli.a nuttalli.along wi.h the new speci.s Alveoli.a ozcani.n. sp. that we i.clude i.to the Alveoli.a elli.ti.a gr.up. We have also found Nummuli.es ur.ni.nsi., Nummuli.es obesus and Nummuli.es cf. ver.eui.i.and associ.ted calcar.ous nannofossi.s that look r.li.ble to make thoughtful cor.elati.ns wi.h the Shallow Benthi. Zones(SBZ). The for.mi.i.er.l bi.str.ti.r.phy suggests an assi.nment to the upper.par. of the lower.Luteti.n-lower.par. of the mi.dle Luteti.n,SBZ13(Mi.dle Eocene), fur.her.str.ngthened thr.ugh the i.enti.i.ati.n of the calcar.ous nannofossi. NP14b-NP15b or.CNE8-CNE10 bi.zones, pr.vi.i.g a soli. cor.elati.n wi.h the global str.ti.r.phi. standar.s.

关键词： Alveoli.a Calcar.ous nannofossi. Centr.l neo-tethys Centr.l iran Mi.dle Eocene Bi.str.ti.r.phy

Petr.logi. evoluti.n of the Gysi.n ophi.li.i. ser.enti.i.es,NW iran

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Acta Geochi.i.a 2024年第5期43卷 996-1011页

作者： Moni. Modjar.ad Donna L.Whi.ney Hadi.Omr.ni Depar.ment of Geology Faculty of SciencesUrmia UniversityUrmiaIran Depar.ment of Ear.h and Envi.onmental Sci.nces University of MinnesotaMinneapolisMNUSA Depar.ment of Geology Faculty of SciencesGolestan UniversityGorgānIran

The Gysi.n ophi.li.e of NW iran i. located at the i.ter.ecti.n of the ophi.li.e belts of SE Tur.ey,NE i.aq,and iran,and pr.vi.es the oppor.uni.y to i.vesti.ate the pr.ser.ed subducti.n and obducti.n hi.tor. of an i.por.ant tectoni. si.e that has not pr.vi.usly been *** ser.enti.i.ed per.0}oti.es of the Gysi.n ophi.li.e contai. the assemblageli.ar.i.e+chr.soti.e+spi.el/Mg-spi.elwi.h r.li.t cli.opyr.xene(di.psi.e)and ver. r.r. r.li.t or.hopyr.xene and *** composi.i.ns of cli.opyr.xenes and spi.els ar. mor. consi.tent wi.h the for.ati.n of the i.fer.ed pr.toli.hhar.bur.i.esi.afor.-ar.or.upr.-subducti.n zone i.stead of an abyssal *** Gysi.n ophi.li.e i. a r.mnant of the Neo-Tethyan ar.-ophi.li.i. system and r.cor.s shallow subducti.n(i.di.ated by the absence of anti.or.0}e)i. the Late Cr.taceous to Paleocene befor.obducti.nalongthr.stfaultsover.heconti.ental *** r.vi.w the spati.l tr.nds of the metamor.hi. gr.de of the Neo-Tethyan ophi.li.es i. thi. r.gi.n and pr.vi.e detai.ed i.for.ati.n about the petr.logy and mi.er.l chemi.tr. of the Gysi.n ophi.li.e.

关键词： Ophi.li.e Neo-Tethyan Gysi.n Ser.enti.i.e iran