âÙÞËÏ× á.à.
íÏÓË×Á, çåïó, 2009 ÇÏÄ, 124 ÓÔÒÁÎÉÃÙ.
ISBN 978-5-89118-453-4
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÷ ÒÁÂÏÔÅ ÐÒÉ×ÏÄÑÔÓÑ ÒÅÚÕÌØÔÁÔÙ ÉÓÓÌÅÄÏ×ÁÎÉÑ ÓÏ×ÒÅÍÅÎÎÏÇÏ ÒÕÄÏÏÂÒÁÚÏ×ÁÎÉÑ × ËÁÌØÄÅÒÅ õÚÏÎ (ëÁÍÞÁÔËÁ). éÓÓÌÅÄÏ×ÁÎÏ ÓÔÒÏÅÎÉÅ ÒÕÄÎÏÇÏ ÔÅÌÁ, ÒÁÓÐÒÅÄÅÌÅÎÉÅ ÜÌÅÍÅÎÔÏ× × ÒÁÚÒÅÚÁÈ. ðÒÉ ÐÏÍÏÝÉ ÏÒÉÇÉÎÁÌØÎÏÊ ÁÐÐÁÒÁÔÕÒÙ ÉÚÍÅÒÅÎÙ ÉÎÔÅÎÓÉ×ÎÙÅ ÐÁÒÁÍÅÔÒÙ ÒÕÄÏÏÂÒÁÚÏ×ÁÎÉÑ: ÔÅÍÐÅÒÁÔÕÒÁ, ËÉÓÌÏÔÎÏÓÔØ ÒÁÓÔ×ÏÒÏ×, ÏËÉÓÌÉÔÅÌØÎÏ-×ÏÓÓÔÁÎÏ×ÉÔÅÌØÎÙÊ ÐÏÔÅÎÃÉÁÌ, ÁËÔÉ×ÎÏÓÔØ ÒÁÓÔ×ÏÒÅÎÎÏÇÏ ÓÅÒÏ×ÏÄÏÒÏÄÁ. éÓÓÌÅÄÏ×ÁÎÏ ÓÏÏÔÎÏÛÅÎÉÅ ÄÅÂÉÔÏ× ÇÁÚÏ×ÏÊ É ÖÉÄËÏÊ ÆÁÚ É ÉÈ ÔÅÐÌÏÓÏÄÅÒÖÁÎÉÅ. îÁ ÏÓÎÏ×Å ÐÒÉÒÏÄÎÙÈ ÎÁÂÌÀÄÅÎÉÊ ÐÏÓÔÒÏÅÎÁ ÔÅÒÍÏÄÉÎÁÍÉÞÅÓËÁÑ ÍÏÄÅÌØ ÇÉÄÒÏÔÅÒÍÁÌØÎÏÇÏ ÐÒÏÃÅÓÓÁ × ËÁÌØÄÅÒÅ õÚÏÎ, × ËÏÔÏÒÏÊ ÕÞÔÅÎÙ ×ÏÚÍÏÖÎÙÅ ÆÁËÔÏÒÙ ÒÕÄÏÏÂÒÁÚÏ×ÁÎÉÑ: ËÉÐÅÎÉÅ, ÓÍÅÛÅÎÉÅ É ÏÈÌÁÖÄÅÎÉÅ É ÏËÉÓÌÅÎÉÑ. áÎÁÌÉÚ ÒÅÚÕÌØÔÁÔÏ× ÔÅÒÍÏÄÉÎÁÍÉÞÅÓËÏÇÏ ÍÏÄÅÌÉÒÏ×ÁÎÉÑ ÓÏÐÏÓÔÁ×ÌÅÎ Ó ÄÁÎÎÙÍÉ ÐÏ ÍÉÎÅÒÁÌÏÇÉÞÅÓËÏÊ ÚÏÎÁÌØÎÏÓÔÉ É ËÏÎÃÅÎÔÒÁÃÉÉ ÆÏÒÍ ÓÅÒÙ, ÞÔÏ ÐÏÚ×ÏÌÉÌÏ ÕÓÔÁÎÏ×ÉÔØ ÒÏÌØ ÒÁÚÌÉÞÎÙÈ ÆÁËÔÏÒÏ× ÒÕÄÏÏÔÌÏÖÅÎÉÑ × ÆÏÒÍÉÒÏ×ÁÎÉÉ ÒÕÄÎÏÊ ÚÁÌÅÖÉ. ðÒÅÄÌÏÖÅÎÁ ÎÏ×ÁÑ ÍÏÄÅÌØ ÒÕÄÏÏÔÌÏÖÅÎÉÑ, ËÏÔÏÒÁÑ ÏÂßÑÓÎÑÅÔ ÆÏÒÍÉÒÏ×ÁÎÉÅ ÐÏÌÎÏÇÏ ÒÕÄÎÏÇÏ ÒÁÚÒÅÚÁ ËÁË ÓÌÅÄÓÔ×ÉÅ ÓÁÍÏÒÁÚ×ÉÔÉÑ ÓÉÓÔÅÍÙ × ÕÓÌÏ×ÉÑÈ ÒÁÚÇÒÕÚËÉ ÔÅÒÍÁÌØÎÙÈ ×ÏÄ. òÁÓÞÅÔÎÙÅ ËÏÎÃÅÎÔÒÁÃÉÉ ÒÁÓÔ×ÏÒÅÎÎÙÈ ÆÏÒÍ ÓÅÒÙ É ÒÕÄÎÙÈ ËÏÍÐÏÎÅÎÔÏ× ÎÁÈÏÄÑÔÓÑ × ÈÏÒÏÛÅÍ ÓÏÇÌÁÓÉÉ Ó ÐÒÉÒÏÄÎÙÍÉ ÄÁÎÎÙÍÉ.
òÅÚÕÌØÔÁÔÙ ÐÒÏ×ÅÄÅÎÎÙÈ ÒÁÂÏÔ ÍÏÇÕÔ ÂÙÔØ ÐÏÌÅÚÎÙ ÐÒÉ ÉÓÓÌÅÄÏ×ÁÎÉÉ ÇÉÄÒÏÔÅÒÍÁÌØÎÙÈ ÍÅÓÔÏÒÏÖÄÅÎÉÊ É ÓÏ×ÒÅÍÅÎÎÙÈ ÇÅÏÔÅÒÍÁÌØÎÙÈ ÓÉÓÔÅÍ.
Bychkov A.Yu. The geochemical model of present-day ore formation in Uzon Caldera (Kamchatka) - Moscow: GEOS, 2009. - 124 p.
The study of present-day hydrothermal ore-forming process in Uzon caldera (Kamchatka, Russia) is reported. The structure of ore body and the distribution components are described. Parameters of ore-forming process (temperature, pH, Eh and activity of dissolved hydrogen sulfide) are measured with original experimental devices. Parameters of gas and liquid phase flow and heat of hydrothermal fluid are studied in details. Base on this investigation results, the thermodynamic model of ore-forming process in Uzon caldera is designed. This model includes several ore-forming mechanisms: boiling, cooling and mixing and oxidization of hydrothermal solution. The analysis of thermodynamic simulation results of is compared with the data on mineralogical data and concentration of forms of sulfur that has allowed establishing a role of various ore-forming factors in ore deposition. The new model of hydrothermal ore process which explains formation of the full ore structure as consequence of self-development of thermal solutions is offered. Calculated concentration of the dissolved forms of sulphur and ore components are in the good consent with the natural data. Results of the spent works can be useful at research of hydrothermal deposits and modern geothermal systems.
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1.1. çÅÏÌÏÇÉÞÅÓËÏÅ ÓÔÒÏÅÎÉÅ
1.2. çÉÄÒÏÔÅÒÍÁÌØÎÁÑ ÄÅÑÔÅÌØÎÏÓÔØ
1.3. óÏ×ÒÅÍÅÎÎÏÅ ÒÕÄÏÏÂÒÁÚÏ×ÁÎÉÅ × ËÁÌØÄÅÒÅ õÚÏÎ É ÅÇÏ ÉÚÕÞÅÎÎÏÓÔØ
1.4. ôÅÒÍÏÄÉÎÁÍÉÞÅÓËÉÅ ÍÏÄÅÌÉ ÓÏ×ÒÅÍÅÎÎÏÇÏ ÒÕÄÏÏÂÒÁÚÏ×ÁÎÉÑ ÎÁ ËÏÎÔÉÎÅÎÔÁÈ
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2.2. ôÅÍÐÅÒÁÔÕÒÎÁÑ ÚÏÎÁÌØÎÏÓÔØ òÕÄÎÏÇÏ ðÏÌÑ
2.3. íÉÎÅÒÁÌÏÇÉÞÅÓËÁÑ ÚÏÎÁÌØÎÏÓÔØ
2.4. ìÉÔÏÈÉÍÉÞÅÓËÁÑ ÚÏÎÁÌØÎÏÓÔØ
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3.2. éÎÔÅÎÓÉ×ÎÙÅ ÐÁÒÁÍÅÔÒÙ ÒÕÄÏÏÂÒÁÚÏ×ÁÎÉÑ ÎÁ õÚÏÎÅ
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4.1. çÒÁÎÉÃÙ ÒÁÓÓÍÁÔÒÉ×ÁÅÍÏÊ ÓÉÓÔÅÍÙ
4.2. ëÏÎÃÅÐÔÕÁÌØÎÙÅ ÍÏÄÅÌÉ ÒÕÄÏÏÂÒÁÚÏ×ÁÎÉÑ
4.3. óÏÓÔÁ×Ù ÇÉÄÒÏÔÅÒÍÁÌØÎÙÈ ÒÁÓÔ×ÏÒÏ× É ÇÁÚÏ×
4.4. óÏÏÔÎÏÛÅÎÉÅ ÄÅÂÉÔÏ× ÇÁÚÁ É ÖÉÄËÏÓÔÉ × ÇÉÄÒÏÔÅÒÍÁÌØÎÙÈ ÆÌÀÉÄÁÈ. ôÅÐÌÏ×ÏÊ ÐÏÔÏË
çÌÁ×Á 5. ôÅÒÍÏÄÉÎÁÍÉÞÅÓËÁÑ ÍÏÄÅÌØ.
5.1. éÓÈÏÄÎÙÅ ÔÅÒÍÏÄÉÎÁÍÉÞÅÓËÉÅ ÄÁÎÎÙÅ
5.2. ëÉÎÅÔÉÞÅÓËÉÅ ÏÇÒÁÎÉÞÅÎÉÑ ÔÅÒÍÏÄÉÎÁÍÉÞÅÓËÏÊ ÍÏÄÅÌÉ
5.3. íÏÄÅÌØ ËÉÐÅÎÉÑ
5.4. íÏÄÅÌØ ÏÈÌÁÖÄÅÎÉÑ
5.5. íÏÄÅÌØ ÏËÉÓÌÅÎÉÑ
5.6. ðÏÌÉÓÕÌØÆÁÎÎÁÑ ÍÏÄÅÌØ ÒÕÄÏÏÂÒÁÚÏ×ÁÎÉÑ
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E-mail: geos@ginras.ru
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