ÓÄÊ 550.41: 553.22
© Ä. ÷ë. À. Â. ÊÓÐÃÓÇÎÂÀ,* ä. ÷ë. Ñ. Ç. ÑÌÈÐÍÎÂ,**
,
***
Þ. È. ÊËÞÊÈÍ,**** Í. Ñ. ÊÀÐÌÀÍÎÂ**
ÂÊËÞ×ÅÍÈß ÁÎÃÀÒÛÕ ÂÈÑÌÓÒÎÌ ÐÀÑÒÂÎÐΠ ÊÂÀÐÖÅ
ÈÇ ÖÂÈÒÒÅÐÎÂ Â ËÈÒÈÉ-ÔÒÎÐÈÑÒÛÕ ÃÐÀÍÈÒÀÕ
ÑÅÂÅÐÍÎÃÎ ÌÀÑÑÈÂÀ (×ÓÊÎÒÊÀ):
ÂÇÃËßÄ ÍÀ ÏÎÂÅÄÅÍÈÅ ÂÈÑÌÓÒÀ
 ÏÐÎÖÅÑÑÀÕ ÃÐÅÉÇÅÍÈÇÀÖÈÈ
* Íàöèîíàëüíûé ìèíåðàëüíî-ñûðüåâîé óíèâåðñèòåò «Ãîðíûé»,
199106, Ñàíêò-Ïåòåðáóðã, 21-ÿ ëèíèÿ, ä. 2;
e-mail: kurguzova.anna@gmail.com
** ÈÃÌ ÑÎ ÐÀÍ, Íîâîñèáèðñê; e-mail: ssmr@uiggm.nsc.ru
*** Íîâîñèáèðñêèé ãîñóäàðñòâåííûé óíèâåðñèòåò, Íîâîñèáèðñê
**** Virginia Polytechnic Institute and State University, Department of Geoscience,
Blacksburg, VA, USA
Äàíà îáùàÿ õàðàêòåðèñòèêà öâèòòåðîîáðàçóþùèõ ôëþèäîâ Ñåâåðíîãî ìàññèâà (×óêîòêà).
Äåòàëüíî ðàññìîòðåíû ôëþèäíûå âêëþ÷åíèÿ â êâàðöå öâèòòåðîâ, ñîäåðæàùèå êðèñòàëëè÷å-
ñêèå ôàçû îêñèãàëîãåíèäîâ âèñìóòà. Ïîëó÷åííûå äàííûå ïîçâîëÿþò ñäåëàòü íåêîòîðûå âûâî-
äû î ôîðìàõ ïåðåíîñà âèñìóòà â ïîñòìàãìàòè÷åñêèõ ôëþèäàõ, ñâÿçàííûõ ñ ëèòèé-ôòîðèñòûìè
ãðàíèòàìè.
Êëþ÷åâûå ñëîâà: öâèòòåðû, ãðåéçåíû, ×óêîòêà, áèñìîêëèò, äîáðåèò, âèñìóò, ôëþèäíûå
âêëþ÷åíèÿ.
A. V. KURGUZOVA, S. Z. SMIRNOV, Yu. I. KLYUKIN, N. S. KARMANOV.
INCLUSIONS OF Bi-RICH SOLUTIONS IN QUARTZ FROM ZWITTERS
IN LITHIUM-FLUORINE GRANITES OF SEVERNYI MASSIF (CHUKOTKA):
INSIGHT INTO THE Bi BEHAVIOR IN GREISENIZATION PROCESSES
There is general characteristic of zwitters-forming fluids of Sevenuy massif (Chukotka). Fluid in-
clusions in quartz from zwitters containing crystalline phases of bismuth oxy-halogenides are descri-
bed in detail. Obtained data lead to some conclusions about forms of the bismuth transport in
post-magmatic fluids connected with lithium-fluorine granites.
Key words: zwitters, greisens, Chukotka, bismoclite, daubreeit, bismuth, fluid inclusions.
 ñòàòüå ïðèâåäåíû ðåçóëüòàòû èññëåäîâàíèé ôëþèäíûõ âêëþ÷åíèé â
êâàðöå öâèòòåðîâ, ãåíåòè÷åñêè ñâÿçàííûõ ñ ëèòèé-ôòîðèñòûìè ãðàíèòàìè
ìàññèâà Ñåâåðíûé (×àóíñêèé ðàéîí ×óêîòêè).  ÷àñòíîñòè, ïðåäñòàâëåíà íî-
âàÿ èíôîðìàöèÿ î íàõîäêå âî ôëþèäíûõ âêëþ÷åíèÿõ îêñèõëîðèäíîãî ñîåäè-
íåíèÿ âèñìóòà. Ïîëó÷åííûå äàííûå ïðåäñòàâëÿþò çíà÷èòåëüíûé èíòåðåñ, ïî-
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2014 ÇÀÏÈÑÊÈ ÐÎÑÑÈÉÑÊÎÃÎ ÌÈÍÅÐÀËÎÃÈ×ÅÑÊÎÃÎ ÎÁÙÅÑÒÂÀ ×. CXLIII, ¹2
2014 ZAPISKI RMO (PROCEEDINGS OF THE RUSSIAN MINERALOGICAL SOCIETY) Pt CXLIII, N2