54 



0. 0. BAEJyH,ir,1>. 



TejibHoe coKpamenic MOJieKyjiapnaro o6xeMa'), KaKi. 6biJio yKaaaHO Bbime, no ycjiOBiaMt ycTofi- 

 qHBOCTH npn BbicoKHX'L xeMnepaiypax^ MneepajiOBT) toh h Apyrofl cxopoHbi ypaBHenifl nejibsfl 

 cocTaBHTb ceS-fe hchoh KapTHHfai pasjHqifl bi ycJIOBiax^ ex% o6pa30Baeifl; Bct noABeprHyxbie 

 ceHiacL pascMOTp'feHiK) lUHHepajibi xapaKTepnbi KaKi ajih nopoAi 3oebi KaxaMopoasMa, xaKi h 

 wa nopoAi HSBepaceHHbixi^). CoKpamenie MOJieKyjiapHaro oGxeMa, iipn oOpasoBaaiH Mnne- 

 pajiOBTj, HaMixHBiiiHx^ HOBoe paBHOB-fecie, Aaeii npaBo npeAnojiaraxb, qxo ycjOBifl HOBaro 

 paBHOB'fecifl, KT. KoxopoMy cxpcMHJiacb CHCxema, BbipaatajiHCb bt> noBbimeHHOMXj AaBJieBie npn 

 cpaBHHxejibHo BbicoKOH eii;e xemnepaxypt. /I,pyrHMH cjoBaMH: HaBasbiBaexca npeAcxaBJieaie o 

 xoMX, qxo BTi ycjiOBiaxi o6pa30BaHia MHHcpajibHbix'L coqexaeiH «pejinKXOBaro)) xapaKxepa 

 r-naBHaa pojib npHHaAJieacajia BbicoKofi xeMnepaxyp-fe, meatAy rkn-b Kani noBbia ycjioBia xapaK- 

 xepnsoBajincb BbicoKHMi, AaBjeHieMT>. pojn AaBJieuia npn oSpasoBaaiH MHHepajiOBi, ocoSeaHO 

 npn BbicoKHxi xGMnepaxypaxi, oieab wajio nsBtcxHO, bo BcaKOMi cjiyqai, aKcnepHMeaxajbebia 

 HSCJifeAOBaaia noKasajiH, qxo oea cHJbHO npeyBejinqeaa^), h gabe jih AaBJieniio mohiho npHnn- 

 caxb 3HaqeHie paBHocHJibHoe, ho HanpaBjeaHoe btj npoxHBonojioatHyK) cxopoay BbicoKHMT> 

 xeiunepaxypaMi. Pojib AaBJieida bi cMbicj-fe pacxBopHMOcxn h Bsaniuearo oSMtna SHaiHTejbHO 

 Jierqe noAJie>KHxi yiexy npn ExowAeniH bi cncxexiy pacxBopaxe^a *), b-b 3xomi cjiyqat boaw; 

 BT> cocxaBT> KopAiepnxa H?e bxoahxi BOAa^), Koxopaa, nrpaa pojb pacxBopuxejia no jtByio cxo- 

 pony ypaBHenifl (cm. Bbiuie), ae bxoahxt> bi ihcjo aesaBncHMbixi KOMnoeeaxoBi CHCXcMbi ^). 



Kt. saaqeaiK) npoACxoamaro pa3cyHJAeHia AJia Bbiacaenia ycJioBia oepaaoBaaia onacan- 

 aaro KopAiepaxoaaro raefica aepaycb aaate. Ocxaexca em,e cKaaaxb o nponcxoacAeuiH ero, 

 xo ecxb o6x HCXOABOMT. Maxepiaji'fc. Bbime, aa ocaoaaaiB cxaxncxaqecKaro Maxepia;ia a npa 

 noMoma nepecqeia aaajiaaa, a BbiCKa3ajica sa Btpoaxaocxb ero ocaAOiaaro npoacxoacAeaia; 

 npocxofi B3rjiaAT> aa xaSjiany IX noAxaepatAaexi axo B033p'feaie a xapaKxepa3yexTi acxoAabia 

 Maxepiajn> KaKi rjiyfioKOBOAHbia (rojiyGoa?) bjiT). Pasaaua bi cxenena oKacjieaia hcoji feaa Aayx^ 

 nopoAt JierKo aaxoAnxT) ceSt oSiacaeaie bi B03CxaB0BJiaK)m,BXT> npoueccaxx., conpoBoatAaio- 

 ui,axT> o6pa30Baaie KopAiepaxoBoa nopoAbi; KaKT> 6yAexT) ynaaaao anate, nopoAW, xoHiecxBeaabia 

 (noBaABMOMy) cb aea ao acxoAHOsiy Maxepiajiy, ao ox.iaqHbia oxii aea no cxeneaa MexaMop*e- 



1) JI,:ia nepBaro ypaBHenin axo coKpamenie Bbipa/Kacx- 

 cji npii6.iii3iiTe.ibno cjli^yiomHMii iiiiciaMii: 294.2 — >• 233, 

 A-iH BToporo: 1085 — > 473; cp. F. Becke, Uber Mineral- 

 bestand und Struktur der kristallinen Schiefer. Denkscbr. 

 Wien. Ak. 75.i (1913, HOBoe H3AaHie), cip. 6 — 25. 



2) J. Johnston and P. Niggli, General principles 

 underlying metamorpbic processes II. Journ. of Geo]., 21 

 (1913), cxp. 588—624. 



3) F. D. Adams, An experimental investigation into 

 the action of ditt'erential pressure on certain minerals and 

 rocks, employing the process suggested by professor Kick. 

 Journ. Geo]., 18 (1910), cxp. 489—525; id.. An experi- 

 mental contribution to the question of the depth of the zone 

 of flow in the earths crust. Ibid. 20 (1912), cxp. 97—116. 



4) Cp. L. H. Adams und J. Johnston, On the effect 

 of high pressures on the physical and chemical behavior 

 of solids. Amer. Joiu-n. Sc. 55 (1913), 205—253. 



5) Ilo Farrington, Penfield, Zambonini u ^p. 



6) Ho npeAnociaHiflM-B, npnHflTLiMi) Bt ocHony iiac.rh- 

 AOBanin A'an't Hoff'a (Zur Bildung der ozeanischeu Salz- 

 ablagerungen I, II. Braunschweig 1905 u. 1909. Yieweg). 

 Kt aHa.iorHiHujit BbiBOAaji-b npnxoAUTTj no oxHOmeHiio 

 MexaMOp'pii'iecKux'b nopoAt bi> HHxepecnoii ii Bcecxopon- 

 nen paCoxh P. Eskola (Om sambandet mellau kemisk 

 och mineralogisk sammansattning hos Orijarvitraktens 

 metamorfa bergarter. Bull. Com. Geol. Finl. JM' 44, Maj 

 1915), c'L. KOTopoii fl noBHai.osiu.icii noijili OKOH'iaaia na- 

 cTOflmaro uacjiAOBaHifl. 



