LITEllATURA ..
1. D'omasze'V'/ska T. - WystE:powanie i eksploa-tacja zlota na Dolnym' SIIlSku. Prz. geol. 1964, nr 4. 2.
ci
a Jew ski Z. - WystE:powanie i wlasno&cimag-nezyt6w .z masywu serpentynitowego Gogol6w -Jorcian6w na tIe budowy geologicznej obszaru. IG
SUMMARY
The nature and geological setting of Ibhe occurreI).-ce of gold in a wea·thering zone of UltramSific Gogo-16w-Jordacaw lIUlIIBif,Lower Siilesia, are cl.iecussed. The Gogolaw-JoIldan6w massif !belongs to a suite of in·trusions 'located along tec·tonic zones deUneating PrecarIibri-an ~elss block of the Sowie Mts.
On the basis of hea;yy-mineral parageneses, -the transfonmatiorui of luHlramaficr0dk6, and ;the
ocour-rence
ofquartz..:feldspar vein deposits, it is assumed that the occutternce of ,gold is connected with the contact zone of grani·toid itntrusion. GoJJd may be an~t metliUogenic index' in studies on perspecti-ve
zones
of this type.Biul. 24D. Z badan zl6Z!lurowcaw skalnych w Pol-sce. T. V, 1970.'
3. G a w r i k 0 waS. N., l.. a r ion 0 w A. M. - Gieo-rogiczeskije i fiziko-chimiczeskije osobiennosti O'b~ ra'2:O'wanija lis'twienitow Kenterlauskogo massiwa. Gleal. Rudn. Miestor.·· 1970, nr 5.
4. G I u c how R. J. - AkkarginskO'je miestoro7.d'ie-· nije zolota. Sow. Gieol. 1971, nr 9.
PB3JOMB
B CTaTJ,e ~aHO' onKcaSHe H xapaltTepHCTKKa YCJlO~
nIDi: .. pacnpO'corpaHeHHS 30JIOTa B Kope BhlBeTpHBaHHSl
nopo~ YJIhTPa6a3HTOBoro MaCCHBa I'orOJIYB-)I!op~aHyn
B . HJOKHeji CHJIe3HH. !3TOT MaCCHB npeH~JIelKHT K KOMnneKcy HBTPY3HBQB, ITPHYPO'IeHBhlX K
TeKTOBH-'1eCKHM 30HaM, o6paMJi.HIOIqHM ~oKeM6pIDl:CKHji rHeji-CO'Bhlji 6JIO'K COBhHX rop.
Ha O'CHOBaHHH lIapareHe3HCa py~HhIX MHBepaJIOB,
H3MeHe~ YJIborpaO'CHO'BBhlX nopo~ (pa3BHTHe JlHCT·· BeHHTOB, TaJIhKHTOs) H npHCYTCTBHH KBapq-lIoJleBO'-wnaTOBhIX lKKJIhHhlX o6pa30sa~ npe~nOJIaraeTCSI,
'ITO 3~eCh paCnpO'CTpaHelia 3O'Ha KOHTaKTa C rpaHHTO-H,lJ;HoA HBTPY3Heji. 3oJlOTO MO'EeT CJIYlKHTh B K8'1eCT-Be BIllKHO'rO MeTaJIJIO'reHH'leCKO'rO KPHTePHSI B
