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Статті в журналах з теми "Allendale Area (N S W )"
Campagnolo, Marcelo, Ricardo Reis, Marcele Santos, Lúcia Kliemann, and Ricardo Savaris. "Which mode and potency of electrocoagulation yields the Smallest Unobstructed Area of the Fallopian Tubes?" Revista Brasileira de Ginecologia e Obstetrícia / RBGO Gynecology and Obstetrics 40, no. 06 (May 29, 2018): 332–37. http://dx.doi.org/10.1055/s-0038-1656718.
Повний текст джерелаSoares, Louis. "Hecke Triangle Groups, Transfer Operators and Hausdorff Dimension." Annales Henri Poincaré 23, no. 4 (October 4, 2021): 1239–81. http://dx.doi.org/10.1007/s00023-021-01117-1.
Повний текст джерелаSoares, Louis. "Hecke Triangle Groups, Transfer Operators and Hausdorff Dimension." Annales Henri Poincaré 23, no. 4 (October 4, 2021): 1239–81. http://dx.doi.org/10.1007/s00023-021-01117-1.
Повний текст джерелаVieira, Antonio José Dias, Dario Alves de Oliveira, Taís Cristina Bastos Soares, Ivan Schuster, Newton Deniz Piovesan, Carlos Alberto Martínez, Everaldo Gonçalves de Barros, and Maurílio Alves Moreira. "Use of the QTL approach to the study of soybean trait relationships in two populations of recombinant inbred lines at the F7 and F8 generations." Brazilian Journal of Plant Physiology 18, no. 2 (June 2006): 281–90. http://dx.doi.org/10.1590/s1677-04202006000200004.
Повний текст джерелаYang, X. B., and F. Feng. "Ranges and Diversity of Soybean Fungal Diseases in North America." Phytopathology® 91, no. 8 (August 2001): 769–75. http://dx.doi.org/10.1094/phyto.2001.91.8.769.
Повний текст джерелаZhao, Zi Qi, Li Guang Li, Hong Bo Wang, Xian Li Zhao, and Peng Jiang. "Characteristics of Land Surface Temperture (LST) within the Third Ring Road of Shenyang." Applied Mechanics and Materials 737 (March 2015): 913–16. http://dx.doi.org/10.4028/www.scientific.net/amm.737.913.
Повний текст джерелаLiu, Anhua, Demin Xu, Michael Henke, Yue Zhang, Yiming Li, Xingan Liu, and Tianlai Li. "Determination of the Optimal Orientation of Chinese Solar Greenhouses Using 3D Light Environment Simulations." Remote Sensing 14, no. 4 (February 14, 2022): 912. http://dx.doi.org/10.3390/rs14040912.
Повний текст джерелаMitsuishi, Mayumi, Simon R. Wallis, Mutsuki Aoya, Jeffrey Lee, and Yu Wang. "E–W extension at 19Ma in the Kung Co area, S. Tibet: Evidence for contemporaneous E–W and N–S extension in the Himalayan orogen." Earth and Planetary Science Letters 325-326 (April 2012): 10–20. http://dx.doi.org/10.1016/j.epsl.2011.11.013.
Повний текст джерелаDelplace, Franck. "An Analytic Form for Riemann Zeta Function at Integer Values." Journal of Mathematics Research 14, no. 6 (November 28, 2022): 1. http://dx.doi.org/10.5539/jmr.v14n6p1.
Повний текст джерелаTirkaamiana, M. Taufan, Lailan Syaufina, and Jumani Jumani. "Growth Analyses of Dipterocarpaceae Stand on Selective Cutting and Line Planting Silvicultural System with Different Planting Line Direction in North Kalimantan." Journal of Tropical Silviculture 13, no. 03 (December 29, 2022): 266–73. http://dx.doi.org/10.29244/j-siltrop.13.03.266-273.
Повний текст джерелаЧастини книг з теми "Allendale Area (N S W )"
James, Simon. "What and Where? Revised Overview of Base Extent." In The Roman Military Base at Dura-Europos, Syria. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780198743569.003.0025.
Повний текст джерелаTikoff, B., P. Kelso, A. K. Fayon, R. Gaschnig, R. M. Russo, J. Vervoort, B. Jicha, and M. J. Kahn. "The jagged western edge of Laurentia: The role of inherited rifted lithospheric structure in subsequent tectonism in the Pacific Northwest." In Laurentia: Turning Points in the Evolution of a Continent. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.1220(22).
Повний текст джерелаJames, Simon. "How Did the Base Work?" In The Roman Military Base at Dura-Europos, Syria. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780198743569.003.0028.
Повний текст джерелаJames, Simon. "The Plateau Zone East of G St." In The Roman Military Base at Dura-Europos, Syria. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780198743569.003.0020.
Повний текст джерелаJames, Simon. "The Wadi Zone Campus, Citadel, and C3 Bath." In The Roman Military Base at Dura-Europos, Syria. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780198743569.003.0021.
Повний текст джерелаHøjerslev, Niels K. "A History of Early Optical Oceanographic Instrument Design in Scandinavia." In Ocean Optics. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195068436.003.0011.
Повний текст джерела"large fluctuation, which usually think grid is resistive obvious or perceptual characteristics of different. Frequency domain analysis of impedance values As can be seen from the test station area topology, in the Tai area, power line wiring is complex, with many branches, and longer. In such a high frequency, signal propagation environment can large fluctuation, which usually think large fluctuation, which usually think grid is r te i sc i ss t o if v e d if ofe b rv e in o tu . s or perceptual characteristics of different. Frequency doma in analysis of es d nn c vm al u ee s Apo s ne f mi a th t es sw ta ae r ea ori p og l o Ti a im ar ay , oa w eh r , i ne wd i r nn g sr . c o ec x mh a ye q b ancy h agn d go e . g I sn u ch av ir h gm h rt e qu y, ss i n al pm ro p nip at e nr m er n tce c es a l fn o r aq ue m ly-ti." In Structural Health Monitoring and Integrity Management, 152–53. CRC Press, 2015. http://dx.doi.org/10.1201/b18510-48.
Повний текст джерела"Jeu as nte -A A u fr g ic uasnt. T lo h w ese in tropospheric jetstr ea le mvc el l , u de antdhew su e b st t ro A pi f c ri aclan ea st m er ildy -, deve s. These fast-moving upper pre Spoa lo re pdendes th srpoou li gch ie s s . ound early warning and disaster ltehveeltw ra inn cieties in sdpsoh rt avoeffamr-o re is atcuhrien , g m im opmaecn ts tuwm it , hproelslpuetcatnttso , reeflfyorh ts e , a w vi h ly icohndp ev o e st l -o dpiisnagstceorurnetlr ie ie fsa , ned sp reech ia alb ly ilA ita fr tiicoan , a an tm dop sp es htesr , ic to dgyentahm er ic w s. ith many other aspects of the tdo is atshtee rs s . evIen re imm ake them m creas peadc ts vuo ln fed ra ro o u re ghatn bility doafnmdsooo re th vulnerable Tropical cyclones have both direct and indirect severe consequences of natural disasters c iet eyrn to a tu t r led to th haeliam ss poacc ia ts t ed onwK ith entyhaensrtarionn fa gll. w T in hdes , doic re ecatniwmapvaecst , saanrdefdoerc la N ra attiuornalofDtihsea st 1e9r90Rseadsuc th ti eon In t ( eIrD na N ti D on R a ) l D by e ca th deeaen xc yescsyicvleonperew cip e ith it iant io th netw ha etstoec rn cu Irnw di haennO th ceeaenffeex ct tsenodfpUrnoim te odteNdaitsiaosn te s. rpTrheevemna ti joonraonbd je cptrievpearoefdInD es NsD th R ro iusgthocolv im er atK ol eongyiac . a l It sh hit the Keny arneccoorod uld be as s t . shTohwen th o a ted ind tino th cayt rect ecflto he fe nce ts ahvaaosileafavbe le rcdo ev n e ce ny dama lo rgp te e, in dgc in otuen rn tr aiteiso , ntaol re adcu ti coen , l os esspo ecially in the cyclone, however, occur when the cyclone is far from often as so acnid at esdocw io it ehconnaotm ur iacld di issa ru st petrisofn li , few , hpircohpea rt ryet it hserceegn io tr n e , butthsetrie ll bayt tra in cttesrtfhee ri n re g g io wniatlh wi tnhdes to n w or a m rd aslh at etlip tu tdoess hi tfhtattheap re o st p -d re is vaaslteenrt re iln ie f and . r T eh haeb se il it cao ti uolnd circ Culloas ti e on patterns of the many developing general ciin rc te urlaac ti t o io nnsohvaevrerbeegeinonoabl winds. the regi soenrvaendd between the cou A n tr n ies the extra-includin egw . th d e im feuntsuiroen re to cu rnraetnucrealocflidm ro at uegh variability, tsryosp te ic masl , wmeiadtlhaetr it u sy dsetewmesstle ik r e li etsh , e N fr oorn th ta lAatn la dntb ic lo coksicn il g tchuerrternatdigtlioobnaallcsopn ac cee -r t n im aebopuattttehrenspootfengtlioablacths, a n is geth in e T la e ti l climate, Ke l o ec n o , nenae st Atlantic pat nyan rai cntfiaolnlsanhdavEeNaSltseor ns b , eeanndobEsuerravse ia dpbaetttw erns. inclu O, quasi-biennial oscillati eoenn , h cl u im madt ing the space-time ch an eaecvteinvtis ti etsh . roSuug ch h e im nv piarcoanrm ac e te nrtiasltidces gr oafdaetx io tre ts are currently subj nembey intraseasonal wave, and so forth. The influence of the of many studies and debates, as reflected in the 19 c9t5sw co a m te prlebxod topographical patterns and the large inland Intergovernmental Pane inland wat ieersbiosdv ie e s ry insc ig lu n d if eicL an ak teinViKce to nryiaa . , w Th h e ic h la h rg aess in c d ie inctaitfe ic d ‘d aisssceesrsnm ib elnet inf olfoncC lim lim a ate Change (IPCC) an area of about 70,000 km2 and is the second largest the recent climate trends l ’ u . eInPcCeCof te change, which freshwater lake in the world. The complex topo ever, that no conclusive evidence ( 1h9u9m5a ) nnaoctteid vi , tiheosw in K gr i a li p m hical patterns include Mt. Kenya, Mt. human-can be derived fo anjaro, and the Great Rift Valley with its accurate inmdeutcheoddscf li omrattheed ch et aencgte io nsiagnnd al s a tt urn ib ti ult io mnoroercaltitm en a d te anptroccheasisnesofcamnobuentoab in ta s i . n D ed e ta fr i o ls of the regional natural/anthropoge f Anyamba 1992, Fremming 1970, manOdg al F lo in 1d9 la 9 te 3 r , acn ha dng ac e cu si rgan te a ls cla im re atanv ic a ilab ( lhe, u m to agne -t ihnedrucweid th ) ad celq im ua attee 1966. tch li e m si ast . ecSheavnegrees , icnocnes lu eddqau ta e n for testing various hypo patterns of extreme clim iantge ces ecvheanntgseosf in htuhmeasnp -a icned -u ti c m ed e like drought, would cDorm ou pgohntenatnsdoofthnear tu erxatl reme climate events are normal h ca ig ll hlfiogrhtceld ea brym th it eigIaPtC io C n . and adaptation policies, as iam nd pacco ts m m of onthpehseenon me n in atew ra o n rl nduwaildceliemvaetreyvyaeraira . b T ili htey men Gtlaolbadlegcroandcae ti ronnapbrooucte ss heusmaannd -i nsduusc ta eidn ab ein li vtiyr on o f m an idn im ad al eqiuna the de atural disasters, however, te drou v g el hotpesdhoccokunatbrs ie osrbw er hserheaveef fi b ci aernettniaetsurlaeld re to so u een Conference th rc ees vita on o rga Enlnivstao ir t most o io nnmeonfs ocioecon t the anUdn it oemd ic Naat ctivi Sustain iaobn le s." In Droughts, 84. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-60.
Повний текст джерела"scto th ara ti rsetc ic te s d ( M mo OdSe ) l . f S or m ec it ahstadnad ta are called model output 1994). The state of ENSO is only one of many factors obs terevveedn SS gi T v en a perfect SRSoTp el feow re sckais ( t 1 -9 9i7 .e ) ., shtohweu (K se r d is hn to aKfuom re acrae st t al t . h1e99I5n ) d . ian summer monsoon m to oid ts elEuNsS ed O -a r t -N t C he E P cu rrent operational atmospheric Ward et al. (1993) discuss the useful level of skill In their study e , la ftoerd ty r -a fi i need vne fa lylspastu te brsn ta snfto ia rlpa ra d c ju ti sctamleun se ts . m of a d tr eop in ic a re l al n o ti r m th e A by f ri tchaenU fo KreM ca e st tse or th ol aotgihcaavleOb ff eiecnee (h xianm dc in aesd ts ) fo bra se th d e on specif e ie a d rs ( oofbsseeravseodn ) alSS fo Trew ca esrtess re in la ctei on 1s9h8i6p . swTih th esgeloabrael ly ladrigsetlry ib ubtaesdedSSoTn , SS st Tatiin st itchaelm ea o ch d el sism imulation wapserrieopde at 1e9d50 th -i 9r4 te . enEa ti cmh es s , e w as hoenraelpSoonue th n t. A O tla vnetrict , hean la dstade re claad ti e v , eltyhesm re aalll -ti EmNeSfOo re ccoam sts u initial co unldaitt io io nnswatso st easrttiemdatwe ith th e s lig mha tl gynid tu if dfee ren otfvhaalviedah te addahisnkdic ll asstismim lar adteotwhiatthotbhtea in seadme fr osm ta t c is rto ic sasl -v av anrp ia re ti doincs ta ble and therefore random atmospheric methods. The chief limitation to further progress is a rai enrfaag ll edf or tion th ca elcm ul oad te e l. thTehebtehsitr te meondseilmeus la ti t m io antseao re flsaecaksoonf ( gJluonbeal th tr roopu ic gahlSSeSpTtefm or beecra ) s . tsAvcaclu id ra f te orfo th re ecawse ts ttgylpoibcaall ly v , a a ri l th ea ocuhghgitvheen seasonal SST pattern. Quite of ENSO would help, but would in most years be well, it sho at w io ends in sem as oodneall re ra piln ic fa altledpa th tt eeronbs se qruvietdeifn al sluffo fi rceiceanst. tsAatrmeoaslp so heu ri scedd , ynbaumtitchaely -m oondleyl -h baavseedusreaf in ul T re hgu io s ns fo rofptrheec ip w it s a ystematic or tlido , n -t rhee la tmesdpaa ti pap ll l y ic var odel pre a d ti i o ct nys in g in biases. skill with lead times of a month or less before the require some kind ions wmoaun ld y r th ai antf al hlusm ea asnoin ty ( Fhoa ll sanidncerteaals . ed1 99 th 1 e ). Istuisscaelpsto ib p il o it s y si b o le f g ki ennderoaf te bdi as byadajuM stm OS ofteacdhjnuisqtumee . n T ts h , e perhaps those tropical west Africa to drought through the pro production of operat einot places a huge bnue rd ed en foorntthhiesg co re vsesrivoevreerdu re c c ti eonntd in ecnaedaers -. coTahsitsalcw ha e n st geAfirn ic a th nefolraensdtM because each time the m na oldd el y n is a m ch ic aanlge fo d r , eacansetwmsoedteo ls f s (e u . r g fa ., ceElb ta ohuinrdaan ry dhGaosnbgee1n99s6 ho ) w to nhbayve se v th e e ra lpo au te tnhtoirasla ne O ed S e statistics must be calculated to provide the to weaken the north African monsoon. More studies nneacleys si d sa s ad ojfu ry Msm tm u e lt n id ts e . c T ad h a is l re en qu se ir m es bltehsetgoe ne orbatta io in natnhdetorfopp ic oasls ib nloer th re g A io fr n ic aalnarnatihnrfo al p l, ogaesniwce ll inafs lu efnocr es on fundamental OiSmp st rao ti vse ti m cs enatnsdtuond th eerssecom re osdtehles , nseuecdh fo as r reg W ion ar sdwe it thaml. a ( r 1 gi 9n9a3l ) seaalssoonadlisrcau in sfsaltlh , e a re sk n il eleo de odt . her tahboosvee . related to the flux adjustments, discussed m tim ad eefboy re c th a e st sff real UK orM th et eeon ro olro th g e ic aasltOBfrfaizcielsw in ectes1e9 as 8o7n . dro Kungohwt le p d re gdeico ti fonEsNS in O m is a n in ysup ff airctisenotffotrher eg w io o n rl adlT se hviesreisa relatively dry area, subject to intermittent lbeescsaium se p o in rt a th n ese regions its influence is either small or Hastenr dartohuagnhdt. c T ol hleasbeorfao to re rs c a ( set . s g , ., asHw as etlelnarsatthho1s9e95b ) y , p ea ro st foBurnad zil an t than other factors. For instance, north are mainly statistical, although real-time dynamical patterns ( lFyo ll iandf lu west A nd eentcael. d frican w 19 b9y1 , H tro ept ic saela so Ant la ra nitn ic fa ll astenrath 1995, WSaSrTeM for eetceaosrtosl og hiacvae ard based on tropi lcbaOlAfefe ic n e . mTahdee st saitn is ctei cal 19f9o4 re ca bsy ts tahreeS1S9T 97 ) i . n In th aeddtirtoipoinc , aplaIrn ts d i of the Sahel are affected by on ENSO SSTs. On tl aanv ti ecraSgSeT , t a ro npoim ca allyAp tl aatn te ti rcnsSaSnTdsF Si o m ll i a la nrd ly , eltocaall . SS 19 T9p1a , tt Bar anns to Onceaannd (P Sam lm ith er11999866 ). , h re agvieonaboofuSt ou tw th ic Aem th e e ri cian , fl aule th nocue gh ofexEtN re SmOeE fo NrStOhs is , A no urstth ra w li eas , tnooftA ab ulsyt ra ilniatih er e ns influence precipitation in such as that in 1982-3, can dominate the circulation Drosdowsky 1993, F n re d th IendA ia uns tr O al c ia enanw north and and precipitation patterns over tropical South ericksen and i B nt aelrgo ( v e. ign . d , A sis m te e n ri t c ly a . h T ig hhe le r v ea el l -t o im f e sk iflol, resc im as itlsarhtaovethhaatdobatac in oend ." In Droughts, 63. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-43.
Повний текст джерела"National Drought Mitigation Center for the forty-eight contiguous states in the United States demon strated that severe and extreme drought affected more than 25 per cent of the country in twenty-seven o of ft7h5e0p ,0 a 0 st 0omnie2h (1 u , n9d4r2e , d50y0 ea k rs m . 2 T ) h o is rrm ep orrees . ents an area con D tr raosutg to htf lo s o el ddso , m hu rrre ic su an lt ess , inansdtrtuoc rn tu ardaol es d . a m Fo argteh , e s in e reasons, the quantification of impacts and the pro vision of disaster relief are far more difficult tasks for A fif lttyho ye uagrhsaT go an , n c ehill’s book was written m drought than they are for other natural hazards. recognising the li omnasteotloogf ists continue to strug o g re le twhiatnhtEommeerdgetnocydem al a in ngagweirtsh , ifm or paecxtasm th p a le t , ar aerestm ru ocrteu ra alccaunsd p cr oiltiecry ia ) m fo ak redresclcaor ntinue tdor ou d g eb hat te a nd th e sc ie bnatsiissts (i a . ned ., lcoocm al m ise udn , i ca re ti sopno nd an in dgttroa ns th peosre ta t e io v n en ts c ha bnynerless , to p ri rnog acc Second, the ab in se gnacneeonfdatopraecdirsoeugahntd . universally vdird in in k g in gemwear te gre , nacnydm so edfiocratlh . s T up h p es li eesc , ha ernascu te r r in is g ti cs sao fe f a it bsoeupttewdh definition of drought adds to the confusion drought have hindered the development of accurate, mu dsetgb re eeeotf her or reg s io ev nerai ty n . oRtneaald is rto ic uag lly h , tdeexfiisntistiaonnds , oiffd it roduogehst , a re nld ia , bl uel , tiamnadtetliym , el tyhee st fiom rm ate u s la o ti fon se voefr it dyraonudgh im tpcaocn ts T th haitshiasvoenbeeeenxpdle an d at iaopnplfiocrattihoens ( coor re im spoafcdt) efsipne it ciio fi ncs . ting Heanzcayrd pl aenvsenbtysm ha ovsetbgeoevnerrnam nk eend ts b . y Bryant (1991) faincaalty io se ndsm tud o y re , th vaenl op 1e5d0 . W de iflihniitte io annsdiGn la th n e tz ir (1 c 9 la 8 ss 5 i ) roannk th in egb is assiusmomftah ri esierdcihnarTaacb te le ri s1t . i1c . sKaenydhiamzp ar adctcsh . aTrh ac is ddeeffiinne it idornosug are annudmemraonuys , mmoarney ex diost. noAtl th ad oeuqguhatteh ly etoefritsh ti ecsdu eg se re defoorftsheivsee ri v ty al , ulaetn io g n th inocf lu edveenatn , e to xtparlesasrieoanlp ar oel ic a y rb m i akers h . t T in hemteharneisnhgofludlstefromrsde fo cl ras ri c n ie gntd is rtosuagnhdteefxfteecn ts t, , tlootnagl -l toesrsm of im li p fe a , ctt , otsauldedceonnnoem ss i , calnod ss , oscoccu ia r lteox am sp pelceitfriacryim in pam ct o s st inc as keesy (i e . ceo ., ntohm ey ic ar seecn to orts ) l . i nk FeodrA re lntcheouogfhatshseocriaattiendgshoafzatrhdesvfao ri rou th s ir htayz -a orndesihnazTaarbdlse . pmeor cent , owfnho at r m is atlhperesc ig ip niitfa ic ti aonnceovoefraatphe re ri sohdolodfo th fr7e5ep1r .1 ova id re essuabnjeicnttievge, rattheedoavsesreaslslm ra ennktiosfuh se afzualrdb ec cahuas ra eci tsee spe nctihas ll yormmio sl reea ? d A in gdeffo in r i ti looncao ti fon th sisw ty it phewa ou st lrdonbgetBee ri csatu ic sseoafntdhetihne te nrse it lya , t io dnusrhaitp io s n , baen tw desepna tia hlaezxatredns. t s ty ta p as eos na olfcporm ob ploenm ent of annual precipitation. These of drought events and the magnitude of associated init n io d n in s g an odftthheelcsaocn are kceopft th beytrheo su c se lt f o or fmau la m ti insgunddeefr icm og pean ct t s , a d rg ruom ug ehntt , ra hnokwsevveerry , h th ig aht . t O ot naelc lo asnsmoafke li fe aaop th p e ly rtshce ie dne ti fsitnsito io rndiin sc a ip clt in oenssiw de il rlateivoenntguiavle ly n n to ee dhotwo associated with drought in this case is significantly assessments of impact in u m al uld ti rpoluegh ec tosn it oum ations (e.g., d ov ro e u rr gah te t d . isLo ra srseoifnl if meo th sattsies tt d in ir gesc . t ly T h as esorcain at keidngwib th yrderlo ie ufgphrtogdreacm la m ra e ti s o ) n . s or revocations for eli igcibsie li cttyortso , dBrroyuagnhtt. atT tr h ib is uitses in a lo pspsroopfr ia li tfeesb in ecceau th se eporfim fa a m ry inceautsoe spre Tahdi rd ov , er draoluag rg hetrigmepoagcrtaspha ic re a nonstruct of famine in recent decades has been civil war or that result from other natural haz laradrse . aFtohraneudraamla and political strife, both of which heighten vulnerability to recent analysis of drought occurrence by x th aemp ( lUeg , eassdS) fa yrsotu em ght. mine s . anDdrocu an ghbteeavesnitgsnid fi icsarnutptnaftouord al p tr riogdguecrtifoonr." In Droughts, 36–37. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-26.
Повний текст джерелаТези доповідей конференцій з теми "Allendale Area (N S W )"
Emanuele, R. M., and J. Fareed. "THE EFFECT OF MOLECULAR WEIGHT ON THE RELATIVE BIOAVAILABILITY OF HEPARIN." In XIth International Congress on Thrombosis and Haemostasis. Schattauer GmbH, 1987. http://dx.doi.org/10.1055/s-0038-1644179.
Повний текст джерелаWitte, Jan, Daniel Trümpy, and Hans Georg Babies. "The Role of Neo-Tectonics in Oil Migration, Lake Turkana Region, Kenya." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2574239-ms.
Повний текст джерелаKrisnabudhi, A. "New Insight Into Berau Sub-Basin North East Borneo: Basin Evolution and Tectonostratigraphy and Their Implication to New Exploration Play Concept." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-g-489.
Повний текст джерелаWhitcomb, Nick, Abdulla Seliem, Rachel Marzen, Bernardo Jose Franco, Maria Agustina Celentano, Sweta Bose, and Alejandra Maldonado Pena. "SE Abu Dhabi Aptian 5 Shuaiba System: Understanding a Heterogeneous Reservoir Trend." In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/207454-ms.
Повний текст джерелаShi, Xuewen, Yanming Tong, Wenping Liu, Chunduan Zhao, Jia Liu, and Jian Fang. "Full-Scale Fracture System Analysis of Shale Reservoir and its Petroleum Significance." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21234-ms.
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