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RMS DPI 2008-1-104-0 http://www.minsoc.ru/2008-1-104-0 Ɉɬɥɢɱɢɹ ɡɨɥɨɬɨ-ɤɜɚɪɰɟɜɵɯ ɢ ɡɨɥɨɬɨ-ɩɨɥɢɫɭɥɶɮɢɞɧɨ-ɤɜɚɪɰɟɜɵɯ ɦɟɫɬɨɪɨɠɞɟɧɢɣ ɐɟɧɬɪɚɥɶɧɨɣ Ʉɨɥɵɦɵ ɩɨ ɬɟɪɦɨɛɚɪɨɝɟɨɯɢɦɢɱɟɫɤɢɦ ɞɚɧɧɵɦ ɋɬɪɭɠɤɨɜ ɋ.Ɏ., Ʉɪɹɠɟɜ ɋ.Ƚ., ɇɚɬɚɥɟɧɤɨ Ɇ.ȼ., Ƚɨɥɭɛɟɜ ɋ.ɘ. ɐɇɂȽɊɂ ɆɉɊ, Ɇɨɫɤɜɚ, Ɋɨɫɫɢɹ, blagmet@tsnigri.ru Contrasting fluid inclusion characteristics of the gold-quartz and gold-sulfidequartz deposits of the Central Kolyma region (NE Russia) Struzhkov S.F., Kryazhev S.G., Natalenko M.V., Golubev S.Yu. TsNIGRI MNR, Moscow, Russia, blagmet@tsnigri.ru Summary. Fluid inclusions were studied in quartz from Au deposits of two types found in the Central Kolyma region of the NE Russia, namely, from metamorphic-hydrothermal Auquartz deposits (Natalka, Verkhny Khakchan, Yugler, Degdekan, and Tokichan deposits), and from intrusive-related Au-sulfide-quartz deposits (Dubach, Pauk, Tautedzhak, and Chumysh deposits). Deposits of various types differ in fluid inclusion compositions and PTX characteristics. These characteristics can be used as an assessment criteria at early exploration stages, particularly in revealing sources of gold placers. ɐɟɧɬɪɚɥɶɧɨ-Ʉɨɥɵɦɫɤɢɣ ɪɟɝɢɨɧ (ɐɄɊ) ɩɪɟɞɫɬɚɜɥɹɟɬ ɫɨɛɨɣ ɧɚɢɛɨɥɟɟ ɛɨɝɚɬɭɸ ɦɟɬɚɥɥɨɝɟɧɢɱɟɫɤɭɸ ɨɛɥɚɫɬɶ ɜ ɩɪɟɞɟɥɚɯ əɧɨ-Ʉɨɥɵɦɫɤɨɣ ɡɨɥɨɬɨɪɨɫɫɵɩɧɨɣ ɩɪɨɜɢɧɰɢɢ. ȼ ɩɨɫɥɟɞɧɢɟ ɝɨɞɵ ɐɄɊ ɩɪɢɨɛɪɟɬɚɟɬ ɱɟɪɬɵ ɡɨɥɨɬɨɪɭɞɧɨɝɨ ɪɚɣɨɧɚ ɦɢɪɨɜɨɝɨ ɤɥɚɫɫɚ ɫ ɩɪɟɨɛɥɚɞɚɸɳɢɦ ɤɪɭɩɧɨɬɨɧɧɚɠɧɵɦ ɬɢɩɨɦ ɦɟɫɬɨɪɨɠɞɟɧɢɣ, ɤ ɱɢɫɥɭ ɤɨɬɨɪɵɯ ɨɬɧɨɫɢɬɫɹ ɨɞɧɨ ɢɡ ɤɪɭɩɧɟɣɲɢɯ ɜ Ɋɨɫɫɢɢ ɡɨɥɨɬɨ-ɤɜɚɪɰɟɜɨɟ ɦɟɫɬɨɪɨɠɞɟɧɢɟ ɇɚɬɚɥɤɚ (ȼ.ȼ.Ɋɭɞɚɤɨɜ, Ɇ.ɉ.Ʉɚɡɢɦɢɪɨɜ, ɋ.Ⱥ.Ƚɪɢɝɨɪɨɜ, 2004), ɚ ɬɚɤɠɟ ɪɹɞ ɟɝɨ ɚɧɚɥɨɝɨɜ − ȼɟɪɯɧɢɣ ɏɚɤɱɚɧ, Ⱦɟɝɞɟɤɚɧ ɢ ɞɪ. Ɋɭɞɧɵɟ ɬɟɥɚ ɷɬɢɯ ɦɟɫɬɨɪɨɠɞɟɧɢɣ ɩɪɟɞɫɬɚɜɥɟɧɵ ɲɬɨɤɜɟɪɤɚɦɢ ɢ ɡɨɧɚɦɢ ɩɪɨɠɢɥɤɨɜɨ-ɜɤɪɚɩɥɟɧɧɵɯ ɪɭɞ ɫ ɧɢɡɤɢɦɢ ɫɨɞɟɪɠɚɧɢɹɦɢ ɡɨɥɨɬɚ ɢ ɛɨɥɶɲɢɦɢ ɡɚɩɚɫɚɦɢ ɪɭɞɵ, ɩɪɢɝɨɞɧɵɦɢ ɞɥɹ ɨɬɤɪɵɬɨɣ ɨɬɪɚɛɨɬɤɢ. Ɇɚɥɨɬɨɧɧɚɠɧɵɟ ɦɟɫɬɨɪɨɠɞɟɧɢɹ ɡɨɥɨɬɨɤɜɚɪɰɟɜɨɣ ɮɨɪɦɚɰɢɢ (ɘɝɥɟɪ, Ɍɨɤɢɱɚɧ ɢ ɞɪ.) ɩɪɟɞɫɬɚɜɥɟɧɵ ɜɵɫɨɤɨɡɨɥɨɬɨɧɨɫɧɵɦɢ ɤɜɚɪɰɟɜɵɦɢ ɠɢɥɚɦɢ, ɤɨɬɨɪɵɟ ɪɚɡɞɟɥɟɧɵ ɛɥɨɤɚɦɢ ɫɥɚɛɨɦɢɧɟɪɚɥɢɡɨɜɚɧɧɵɯ ɛɟɡɪɭɞɧɵɯ ɩɨɪɨɞ ɢ ɩɪɢɝɨɞɧɵ ɞɥɹ ɩɨɞɡɟɦɧɨɣ ɢɥɢ ɤɨɦɛɢɧɢɪɨɜɚɧɧɨɣ ɨɬɪɚɛɨɬɤɢ. Ʉ ɩɟɪɫɩɟɤɬɢɜɧɵɦ ɤɪɭɩɧɨɬɨɧɧɚɠɧɵɦ ɨɛɴɟɤɬɚɦ ɨɬɧɨɫɹɬɫɹ ɬɚɤɠɟ «ɧɟɬɪɚɞɢɰɢɨɧɧɵɟ» ɞɥɹ ɪɟɝɢɨɧɚ ɦɟɫɬɨɪɨɠɞɟɧɢɹ ɡɨɥɨɬɨ-ɩɨɥɢɫɭɥɶɮɢɞɧɨ-ɤɜɚɪɰɟɜɨɣ ɮɨɪɦɚɰɢɢ, ɩɪɟɞɫɬɚɜɥɹɸɳɢɟ ɫɨɛɨɣ ɲɬɨɤɜɟɪɤɢ, ɫɜɹɡɚɧɧɵɟ ɫ ɢɧɬɪɭɡɢɹɦɢ ɝɪɚɧɢɬɨɢɞɨɜ (Ⱦɭɛɚɱ, ɉɚɭɤ, Ɍɷɭɬɷɞɠɚɤ, ɑɭɦɵɲ ɢ ɞɪ.). Ɉɩɪɟɞɟɥɟɧɢɟ ɤɪɢɬɟɪɢɟɜ ɢɞɟɧɬɢɮɢɤɚɰɢɢ ɬɢɩɚ ɡɨɥɨɬɨɣ ɦɢɧɟɪɚɥɢɡɚɰɢɢ ɩɨɡɜɨɥɢɬ ɩɪɨɜɨɞɢɬɶ ɜɵɛɨɪ ɩɟɪɜɨɨɱɟɪɟɞɧɵɯ ɨɛɴɟɤɬɨɜ ɢ ɩɨɞɛɨɪ ɚɞɟɤɜɚɬɧɵɯ ɩɪɨɝɧɨɡɧɨ-ɩɨɢɫɤɨɜɵɯ ɦɨɞɟɥɟɣ ɧɚ ɪɚɧɧɢɯ ɷɬɚɩɚɯ ɝɟɨɥɨɝɨɪɚɡɜɟɞɨɱɧɵɯ ɪɚɛɨɬ. Ⱦɥɹ ɪɟɲɟɧɢɹ ɩɨɫɬɚɜɥɟɧɧɨɣ ɡɚɞɚɱɢ ɚɜɬɨɪɚɦɢ ɢɡɭɱɟɧɵ ɮɥɸɢɞɧɵɟ ɜɤɥɸɱɟɧɢɹ ɜ ɡɨɥɨɬɨɧɨɫɧɨɦ ɤɜɚɪɰɟ ɷɬɚɥɨɧɧɵɯ ɦɟɫɬɨɪɨɠɞɟɧɢɣ ɧɚɡɜɚɧɧɵɯ ɪɭɞɧɨ-ɮɨɪɦɚɰɢɨɧɧɵɯ ɢ ɝɟɨɥɨɝɨ-ɩɪɨɦɵɲɥɟɧɧɵɯ ɬɢɩɨɜ (ɪɢɫɭɧɨɤ). Ɉɩɪɟɞɟɥɟɧɵ ɬɟɦɩɟɪɚɬɭɪɵ: ɷɜɬɟɤɬɢɤɢ (Ɍɷɜɬ), ɩɥɚɜɥɟɧɢɹ ɥɶɞɚ (Ɍɩɥ ɥɶɞɚ), ɩɥɚɜɥɟɧɢɹ ɝɚɡɨɝɢɞɪɚɬɚ (Ɍɩɥ ȽȽ), ɩɥɚɜɥɟɧɢɹ ɭɝɥɟɤɢɫɥɨɬɵ (Ɍɩɥ ɋɈ2), ɩɥɚɜɥɟɧɢɹ NaCl (Ɍɩɥ NaCl), ɝɨɦɨɝɟɧɢɡɚɰɢɢ (Ɍɝ). Ɉɛɨɛɳɟɧɧɵɟ ɪɟɡɭɥɶɬɚɬɵ ɤɪɢɨɦɟɬɪɢɱɟɫɤɢɯ ɢ ɬɟɪɦɨɦɟɬɪɢɱɟɫɤɢɯ ɢɫɫɥɟɞɨɜɚɧɢɣ ɩɪɟɞɫɬɚɜɥɟɧɵ ɜ ɬɚɛɥɢɰɚɯ 1−3. ɋɢɦɜɨɥ «ɧ» ɨɡɧɚɱɚɟɬ, ɱɬɨ ɫɨɨɬɜɟɬɫɬɜɭɸɳɢɣ ɮɚɡɨɜɵɣ ɩɟɪɟɯɨɞ ɨɬɫɭɬɫɬɜɭɟɬ ɢɥɢ ɧɟɹɫɧɨ ɜɵɪɚɠɟɧ. Ʉɚɠɞɚɹ ɫɬɪɨɤɚ ɜ ɬɚɛɥɢɰɚɯ ɯɚɪɚɤɬɟɪɢɡɭɟɬ ɝɪɭɩɩɭ ɜɤɥɸɱɟɧɢɣ (ɧɟ ɦɟɧɟɟ 10 ɲɬ) ɫ ɛɥɢɡɤɢɦɢ ɊɌɏ-ɩɚɪɚɦɟɬɪɚɦɢ, ɩɪɢɫɭɬɫɬɜɭɸɳɢɯ ɜ ɨɞɧɨɦ ɢɥɢ ɧɟɫɤɨɥɶɤɢɯ ɨɛɪɚɡɰɚɯ. ȼɫɟɝɨ ɩɪɨɚɧɚɥɢɡɢɪɨɜɚɧɨ ɛɨɥɟɟ 500 ɢɧɞɢɜɢɞɭɚɥɶɧɵɯ ɜɚɤɭɨɥɟɣ. Ɉɛɪɚɡɰɵ, ɫɨɞɟɪɠɚɳɢɟ ɬɨɥɶɤɨ ɦɟɥɤɢɟ ɮɥɸɢɞɧɵɟ ɜɤɥɸɱɟɧɢɹ (< 5 ɦɤɦ) ɢɡɭɱɟɧɵ ɦɟɬɨɞɚɦɢ ɜɨɞɧɵɯ ɜɵɬɹɠɟɤ (20 ɚɧ.) ɢ ɝɚɡɨɜɨɣ ɯɪɨɦɚɬɨɝɪɚɮɢɢ (40 ɚɧ.). ɉɪɢ ɢɧɬɟɪɩɪɟɬɚɰɢɢ ɪɟɡɭɥɶɬɚɬɨɜ ɢɫɩɨɥɶɡɨɜɚɧɵ ɷɤɫɩɟɪɢɦɟɧɬɚɥɶɧɵɟ ɢ ɪɚɫɱɟɬɧɵɟ ɞɚɧɧɵɟ ɩɨ ɫɢɫɬɟɦɚɦ H2O-NaCl, H2O-CO2-NaCl, ɋɈ2-ɋɇ4 (Ɋɟɞɞɟɪ, 1987; Bodnar, Vityk, 1994; Darling, 1991; Thiery et. al, 1994; Bakker, 2003). ɋɨɞɟɪɠɚɧɢɟ ɝɚɡɨɜ ɏ(ɋɈ2+ɋɇ4), ɦɨɥɶ. %, ɪɚɫɫɱɢɬɚɧɨ ɫ ɭɱɟɬɨɦ ɩɥɨɬɧɨɫɬɢ ɝɚɡɨɨɛɪɚɡɧɨɣ ɮɚɡɵ ɢ ɟɟ ɨɬɧɨɫɢɬɟɥɶɧɨɝɨ ɨɛɴɟɦɚ ɜ ɜɚɤɭɨɥɹɯ. 124 Ɋɢɫ.1. Ɍɢɩɵ ɮɥɸɢɞɧɵɯ ɜɤɥɸɱɟɧɢɣ ɜ ɤɜɚɪɰɟ ɡɨɥɨɬɨɪɭɞɧɵɯ ɦɟɫɬɨɪɨɠɞɟɧɢɣ ɐɟɧɬɪɚɥɶɧɨɣ Ʉɨɥɵɦɵ. Ⱥ– ɡɨɥɨɬɨ-ɤɜɚɪɰɟɜɵɟ ɦɟɫɬɨɪɨɠɞɟɧɢɹ: LC− ɜɨɞɧɵɣ ɪɚɫɬɜɨɪ+ɠɢɞɤɚɹ ɢ/ɢɥɢ ɝɚɡɨɨɛɪɚɡɧɚɹ ɋɈ2 ɫ ɩɪɢɦɟɫɶɸ ɋɇ4; L− ɜɨɞɧɨɫɨɥɟɜɨɣ ɪɚɫɬɜɨɪ; ɋ− ɠɢɞɤɚɹ ɢ/ɢɥɢ ɝɚɡɨɨɛɪɚɡɧɚɹ ɋɈ2 (±ɋɇ4,ɇ2Ɉ); Ȼ− ɡɨɥɨɬɨ-ɩɨɥɢɫɭɥɶɮɢɞɧɨ-ɤɜɚɪɰɟɜɵɟ ɦɟɫɬɨɪɨɠɞɟɧɢɹ. ȼɤɥɸɱɟɧɢɹ ɪɚɫɫɨɥɨɜ-ɪɚɫɩɥɚɜɨɜ ɫ ɤɪɢɫɬɚɥɥɨɦ NaCl ɢ ɬɜɟɪɞɵɦɢ ɞɨɱɟɪɧɢɦɢ ɮɚɡɚɦɢ: Ʉ– ɦɢɧɟɪɚɥ ɫ ɫɢɥɶɧɵɦ ɞɜɭɩɪɟɥɨɦɥɟɧɢɟɦ (ɤɚɪɛɨɧɚɬ, ɛɨɪɚɬ?); P– ɩɥɚɫɬɢɧɱɚɬɵɣ ɝɟɤɫɚɝɨɧɚɥɶɧɵɣ ɦɢɧɟɪɚɥ, R– ɬɨɱɟɱɧɚɹ ɪɭɞɧɚɹ ɮɚɡɚ, S– ɞɪɭɝɢɟ ɧɟɪɚɫɬɜɨɪɢɦɵɟ ɦɢɧɟɪɚɥɵ-ɭɡɧɢɤɢ. Ƚɚɡɨɜɨ-ɠɢɞɤɢɟ ɜɤɥɸɱɟɧɢɹ: LC (LCK)− ɜɨɞɧɵɣ ɪɚɫɬɜɨɪ+ɝɚɡɨɨɛɪɚɡɧɵɣ ɋɇ4 ɫ ɩɪɢɦɟɫɶɸ ɋɈ2, ɢ ɫ ɞɨɱɟɪɧɟɣ ɮɚɡɨɣ «Ʉ»; L− ɯɥɨɪɢɞɧɵɣ ɪɚɫɫɨɥ. C– ɜɤɥɸɱɟɧɢɹ, ɫɨɞɟɪɠɚɳɢɟ ɝɚɡɨɨɛɪɚɡɧɵɣ ɢ/ɢɥɢ ɠɢɞɤɢɣ (ɩɪɢ Ɍ<−82°ɋ) ɋɇ4 ɫ ɩɪɢɦɟɫɶɸ ɋɈ2 (ɜɨɡɦɨɠɧɨ, N2); N– ɝɚɡɨɨɛɪɚɡɧɵɟ ɜɤɥɸɱɟɧɢɹ ɧɟɨɩɪɟɞɟɥɟɧɧɨɝɨ ɫɨɫɬɚɜɚ (ɝɨɦɨɝɟɧɧɵɟ ɞɨ −195°ɋ). Fig.1. Fluid inclusions in quartz from Au deposits of the Central Kolyma region. A− gold-quartz deposits. LC− aqueous solution+liquid or gaseous ɋɈ2 with minor ɋɇ4; L− aqueous solution; ɋ− liquid and/or gaseous ɋɈ2 (± ɋɇ4, ɇ2Ɉ). Ȼ − gold sulfide quartz deposits: Brine-melt inclusions with NaCl crystal and solid daughter phases: K− a mineral with a high birefringence (carbonate or borate), P− hexagonal lamellar mineral, R− small ore phase, S− other insoluble minerals. Gas-liquid inclusions: LC (LCK) − aqueous solution+ gaseous ɋɇ4 with minor ɋɈ2, and daughter phase “K”; L− chlorine brine. C– inclusions with gaseous and/or liquid (at Ɍ<−82°ɋ) ɋɇ4 with minor ɋɈ2 (possible N2); N– gaseous inclusions of uncertain composition (homogeneous till −195°ɋ). Ɍɚɛɥɢɰɚ 1. ɏɚɪɚɤɬɟɪɢɫɬɢɤɢ ɜɤɥɸɱɟɧɢɣ ɯɥɨɪɢɞɧɵɯ ɪɚɫɫɨɥɨɜ-ɪɚɫɩɥɚɜɨɜ Ɇɟɫɬɨɪɨɠɞɟɧɢɹ ɉɚɭɤ Ɍɷɭɬɟɞɠɚɤ ɑɭɦɵɲ Ⱦɨɱɟɪɧɢɟ ɮɚɡɵ Ɍɟɦɩɟɪɚɬɭɪɵ ɮɚɡɨɜɵɯ ɩɟɪɟɯɨɞɨɜ, °ɋ Ɋɚɫɱɟɬɧɵɟ ɩɚɪɚɦɟɬɪɵ (ɫɦ. ɪɢɫɭɧɨɤ) Ɍɷɜɬ Ɍɩɥ NaCl %-ɷɤɜ. NaCl Ɋ ɤɛɚɪ Ɍɝ ɀ−Ƚ NaCl+K+R+S NaCl+K+S NaCl NaCl+K+R+P NaCl NaCl+K −55 −55 −55 −55 −38 −55 140−280 270−290 160−170 265−275 140−145 215−250 470−560 280−390 220−290 355−360 250−255 190−200 55.8 − 68.2 36.7 − 46.4 32.9 − 37.4 42.9 − 43.3 34.7 − 35.0 31.4 − 31.9 0.9 1.0 0.8 0.9 - Ɍɚɛɥɢɰɚ 2. ɏɚɪɚɤɬɟɪɢɫɬɢɤɢ ɝɚɡɨɜɵɯ ɜɤɥɸɱɟɧɢɣ (ɬɢɩ «ɋ») Ɇɟɫɬɨɪɨɠɞɟɧɢɹ Ɂɨɥɨɬɨɤɜɚɪɰɟɜɵɟ ɇɚɬɚɥɤɚ Ⱦɟɝɞɟɤɚɧ ȼ.ɏɚɤɱɚɧ Ɍɨɤɢɱɚɧ Ɂɨɥɨɬɨ-ɩɨɥɢɫɭɥɶɮɢɞɧɨɤɜɚɪɰɟɜɵɟ ɘɝɥɟɪ Ⱦɭɛɚɱ ɑɭɦɵɲ ɉɚɭɤ Ɍɷɭɬɟɞɠɚɤ Ɇɨɞɟɥɶɧɵɟ ɩɚɪɚɦɟɬɪɵ Ɏɚɡɨɜɵɟ ɩɟɪɟɯɨɞɵ, °ɋ Ɍɩɥ ɋɈ2 Ɍɝ (Ɏɚɡɚ) Ȟ, ɫɦ3/ɦɨɥɶ X CH4 Ɍɨɛɪ, °ɋ Ɋ, ɤɛɚɪ −57.8 −58.2 −58.5 −56.7 −59.0 −59.5 −61.0 −80 −77 −67.5 ɇɟɬ ɇɟɬ −96 +24.0 (ɀ) +19.0 (ɀ) +16.8 (ɀ) +15.5 (ɀ) +20.0 (ɀ) +17.7 (ɀ) +10.4 (Ƚ) −110 (ɀ) −94.5 (ɀ) −36.5 (ɀ) −88 (Ƚ) –120 (Ƚ) −96 (Ƚ) 70 60 60 54 70−80 75−80 80−90 45 50 <60 200 850 >250 0.05 0.06 0.07 0.00 0.10 0.12 0.22 0.85 0.85 >0.60 1.00 1.00 0.95 300−330 280−290 220−280 295−305 200−225 250−350 350−380 230−270 300−350 265−315 250−300 380−430 350−550 0.8−0.9 1.0 0.8−1.0 1.5−1.6 0.4−0.5 0.5−0.7 0.5−0.7 2.5 2.2−2.4 >1.2 >0.9 >0.1 >0.2 125 Ɍɚɛɥɢɰɚ 3. ɏɚɪɚɤɬɟɪɢɫɬɢɤɢ ɝɚɡɨɜɨ-ɠɢɞɤɢɯ ɜɤɥɸɱɟɧɢɣ (ɬɢɩɵ LC ɢ L) Ɇɟɫɬɨɪɨɠɞɟɧɢɹ Ɂɨɥɨɬɨ-ɤɜɚɪɰɟɜɵɟ ɇɚɬɚɥɤɚ ȼ.ɏɚɤɱɚɧ Ⱦɟɝɞɟɤɚɧ Ɍɨɤɢɱɚɧ Ɂɨɥɨɬɨ-ɩɨɥɢɫɭɥɶɮɢɞɧɨ-ɤɜɚɪɰɟɜɵɟ ɘɝɥɟɪ ɑɭɦɵɲ Ⱦɭɛɚɱ Ɍɷɭɬɟɞɠɚɤ ɉɚɭɤ Ɍɢɩ Ƚɀȼ LC LC LC L L LC LC LC L L LC LC LC L L LC LC LC L L L L LC LC LC L L L LC L LCK LCK LC L LNK LNK LC L Ɍɟɦɩɟɪɚɬɭɪɵ ɮɚɡɨɜɵɯ ɩɟɪɟɯɨɞɨɜ, °ɋ Tɝ Ɍɝ ɋɈ2 Ɍɩɥ. Ɍɩɥ Ɍɩɥ Ɍɷɜɬ (Ɏɚɡɚ) ɥɶɞɚ ȽȽ ɋɈ2 (ɀ−Ƚ) ɧ 7.5 26 (ɀ) −3.5 −57.8 300−330 ɧ ɧ 6.5 23 (ɀ) −57.9 270−290 8 20 (Ƚ) −8 −4.0 −56.7 230−250 ɧ ɧ ɧ −7 −4.8 215−225 ɧ ɧ ɧ −6 −3.2 165−190 ɧ ɧ 7 ɧ ɧ 330−350 ɧ ɧ 7.5 −56.7 16.2 (ɀ) 295−305 ɧ 7 21.0 (Ƚ) −12 −56.9 245−265 ɧ ɧ ɧ −15 −4.3 240−250 ɧ ɧ ɧ −10 −3.8 190−200 ɧ 8.5 −7.5 −58.5 17.5 (ɀ) 270−280 ɧ 8.5 −7.5 −58.0 24.5 (ɀ) 220−230 ɧ 7.2 ɧ ɧ −3.3 200−225 ɧ ɧ ɧ ɧ −4.8 165−175 ɧ ɧ ɧ −12.5 −4.8 210−220 ɧ ɧ ɧ −10 (Ƚ) 380−390 −63.7 ɧ ɧ 7 8 (ɀ) −61.5 350−380 ɧ ɧ 8 ɧ ɧ 250−315 ɧ ɧ ɧ −6 −2.2 340−365 ɧ ɧ ɧ −10 −7.4 310−320 ɧ ɧ ɧ −12 −5.5 235−245 ɧ ɧ ɧ −6 −3 190−225 ɧ ɧ 11.7 ɧ ɧ 365−380 2.8 ɧ ɧ −27 −12.5 330−340 ɧ 5.5 ɧ ɧ −26 290−315 ɧ ɧ ɧ −29 −10.5 290−315 ɧ ɧ ɧ −27 −11.5 240−280 ɧ ɧ ɧ −29 −18.7 190−230 ɧ ɧ 11.5 ɧ ɧ 280−300 ɧ ɧ ɧ −45 −24.5 215−220 ɧ ɧ 4 ɧ ɧ 530−545 ɧ ɧ ɧ −27 −3.3 335−345 ɧ ɧ ɧ −33 −4.8 255−265 ɧ ɧ ɧ −40 −25 190−210 ɧ ɧ ɧ 430−440 −29 −10.4 ɧ ɧ ɧ −29 −11.0 360−390 ɧ +1 ɧ ɧ −8.2 280−290 ɧ ɧ ɧ −55 −29.0 160−170 Ɋɚɫɱɟɬɧɵɟ: %-ɷɤɜ. ɦɨɥ.% NaCl CO2+CH4 5.3 10−11 6.6 5−7 5.2 2 7.9 5.0 5.8 4.9 12−14 5.8 3−4 6.9 6.2 3.0 15−17 3.0 5−6 5.4 3.5−4 7.6 7.6 10−13 5.8 6−8 4.5 2−4 3.7 11.0 8.5 5.0 14.3 8.3 14.5 15.5 21.3 >23 10.5 18.9 20.3 >23 13.9 15.0 13.1 >23 - Ɂɨɥɨɬɨ-ɤɜɚɪɰɟɜɵɟ ɦɟɫɬɨɪɨɠɞɟɧɢɹ ɩɨ ɬɟɪɦɨɛɚɪɨɝɟɨɯɢɦɢɱɟɫɤɢɦ ɩɚɪɚɦɟɬɪɚɦ ɜ ɫɜɨɸ ɨɱɟɪɟɞɶ ɦɨɝɭɬ ɛɵɬɶ ɞɢɮɮɟɪɟɧɰɢɪɨɜɚɧɵ ɧɚ ɲɬɨɤɜɟɪɤɨɜɵɟ ɢ ɠɢɥɶɧɵɟ. ɂɫɫɥɟɞɨɜɚɧɢɹ ɩɨɤɚɡɚɥɢ, ɱɬɨ ɫɪɚɜɧɢɜɚɟɦɵɟ ɡɨɥɨɬɨɪɭɞɧɵɟ ɨɛɴɟɤɬɵ ɨɬɥɢɱɚɸɬɫɹ ɩɪɚɤɬɢɱɟɫɤɢ ɩɨ ɜɫɟɦɭ ɤɨɦɩɥɟɤɫɭ ɬɟɪɦɨɛɚɪɨɝɟɨɯɢɦɢɱɟɫɤɢɯ ɩɚɪɚɦɟɬɪɨɜ. Ɉɫɧɨɜɧɵɦ ɤɪɢɬɟɪɢɟɦ ɢɞɟɧɬɢɮɢɤɚɰɢɢ ɪɭɞɧɨ-ɮɨɪɦɚɰɢɨɧɧɨɝɨ ɬɢɩɚ ɦɟɫɬɨɪɨɠɞɟɧɢɣ ɹɜɥɹɟɬɫɹ ɫɨɫɬɚɜ ɪɭɞɨɨɛɪɚɡɭɸɳɢɯ ɮɥɸɢɞɨɜ, ɤɨɬɨɪɵɣ ɨɬɪɚɠɚɟɬ ɝɟɧɟɬɢɱɟɫɤɭɸ ɫɜɹɡɶ ɨɪɭɞɟɧɟɧɢɹ ɫ ɚɫɫɨɰɢɢɪɭɸɳɢɦɢ ɝɟɨɥɨɝɢɱɟɫɤɢɦɢ ɮɨɪɦɚɰɢɹɦɢ. Ɂɨɥɨɬɨ-ɩɨɥɢɫɭɥɶɮɢɞɧɨ-ɤɜɚɪɰɟɜɵɟ ɨɛɴɟɤɬɵ ɫɮɨɪɦɢɪɨɜɚɧɵ ɩɪɢ ɭɱɚɫɬɢɢ ɜɨɫɫɬɚɧɨɜɥɟɧɧɵɯ ɦɚɝɦɚɬɨɝɟɧɧɵɯ ɯɥɨɪɢɞɧɵɯ 126 ɪɚɫɫɨɥɨɜ. Ɇɟɬɚɦɨɪɮɨɝɟɧɧɨ-ɝɢɞɪɨɬɟɪɦɚɥɶɧɨɟ ɨɪɭɞɟɧɟɧɢɟ ɡɨɥɨɬɨ-ɤɜɚɪɰɟɜɨɝɨ ɬɢɩɚ ɫɜɹɡɚɧɨ ɫ ɪɚɡɛɚɜɥɟɧɧɵɦɢ ɭɝɥɟɤɢɫɥɨɬɧɨ-ɝɢɞɪɨɤɚɪɛɨɧɚɬɧɵɦɢ ɪɚɫɬɜɨɪɚɦɢ (ɬɚɛɥ. 4). Ɍɚɛɥɢɰɚ 4. ɋɪɚɜɧɢɬɟɥɶɧɚɹ ɬɟɪɦɨɛɚɪɨɝɟɨɯɢɦɢɱɟɫɤɚɹ ɯɚɪɚɤɬɟɪɢɫɬɢɤɚ ɡɨɥɨɬɨɪɭɞɧɵɯ ɨɛɴɟɤɬɨɜ ɐɄɊ. Ɍɢɩɵ ɡɨɥɨɬɨɪɭɞɧɵɯ ɦɟɫɬɨɪɨɠɞɟɧɢɣ ɐɄɊ ɉɚɪɚɦɟɬɪɵ ɜɤɥɸɱɟɧɢɣ ɁɨɥɨɬɨɁɨɥɨɬɨ - ɤɜɚɪɰɟɜɵɣ (Ɍ °ɋ ɮɚɡɨɜɵɯ ɩɟɪɟɯɨɞɨɜ ɩɨɥɢɫɭɥɶɮɢɞɧɨɢ ɞɪɭɝɢɟ ɢɧɞɢɤɚɬɨɪɧɵɟ Ʉɪɭɩɧɨɬɨɧɧɚɠɧɵɣ Ɇɚɥɨɬɨɧɧɚɠɧɵɣ ɤɜɚɪɰɟɜɵɣ ɩɨɤɚɡɚɬɟɥɢ) (ɲɬɨɤɜɟɪɤɨɜɵɣ) (ɠɢɥɶɧɵɣ) ɂɧɞɢɤɚɬɨɪɧɵɟ ɮɚɡɵ Ɇɢɧɟɪɚɥɵ-ɭɡɧɢɤɢ ɀɢɞɤɚɹ ɋɈ2 ɏɥɨɪ-ɢɨɧ ɜ ɜɨɞɧɵɯ ɜɵɬɹɠɤɚɯ ȿɫɬɶ ɇɟɬ ɍɝɥɟɤɢɫɥɨɬɧɨ-ɜɨɞɧɵɟ ɜɤɥɸɱɟɧɢɹ Ɍ ɷɜɬɟɤɬɢɤɢ −26…−29 −8…−12 Ɍ ɩɥɚɜɥɟɧɢɹ ɝɚɡɨɝɢɞɪɚɬɚ < 6, >11 6.0…8.5 Ɍ ɩɥɚɜɥɟɧɢɹ ɋɈ2 −56.6…−58.5 −61.5…−63.7 ȼɤɥɸɱɟɧɢɣ ɫ Ɍ ɝɨɦɨɝɟɧɢɡɚɰɢɢ ɝɚɡɨɜɨɣ ɮɚɡɵ > 16 <8 ɠɢɞɤɨɣ ɋɈ2 ɧɟɬ Ɍ ɩɨɥɧɨɣ ɝɨɦɨɝɟɧɢɡɚɰɢɢ 220−330 350−390 ȼɨɞɧɨ-ɫɨɥɟɜɵɟ ɜɤɥɸɱɟɧɢɹ Ɍ ɷɜɬɟɤɬɢɤɢ −27…−55 −5…−15 Ɍ ɩɥɚɜɥɟɧɢɹ ɥɶɞɚ −10… −29 −3.3…−5.0 −2.2…−7.4 Ɉɛɳɢɣ ɞɢɚɩɚɡɨɧ Ɍ ɝɨɦɨɝɟɧɢɡɚɰɢɢ 165−315 165−250 165−365 Ƚɚɡɨɨɛɪɚɡɧɵɟ ɜɤɥɸɱɟɧɢɹ Ɍ ɩɥɚɜɥɟɧɢɹ ɋɈ2 −67… −96 −56.7… −58.5 −59.0…−61.0 Ɍ ɝɨɦɨɝɟɧɢɡɚɰɢɢ (ɮɚɡɚ) 15…25 (ɀ) 10…20 (ɀ, Ƚ) < −36 (ɀ, Ƚ) ɋɨɞɟɪɠɚɧɢɟ CH4 (ɦɨɥɶɧ. %) 0–7 60−100 10−22 V (CO2+CH4), ɫɦ3 / ɦɨɥɶ < 60… >200 50–70 70−90 ɋɈ2/ɋɇ4 (ɯɪɨɦɚɬɨɝɪɚɮɢɹ) 0.1 – 20 0.1 − 1 20 − 100 Ɋɟɡɭɥɶɬɚɬɵ ɢɫɫɥɟɞɨɜɚɧɢɹ ɮɥɸɢɞɧɵɯ ɜɤɥɸɱɟɧɢɣ ɫɜɢɞɟɬɟɥɶɫɬɜɭɸɬ ɨ ɬɨɦ, ɱɬɨ ɧɚ ɦɟɫɬɨɪɨɠɞɟɧɢɹɯ ɷɬɨɝɨ ɬɢɩɚ ɝɥɚɜɧɨɣ ɩɪɢɱɢɧɨɣ ɪɭɞɨɨɬɥɨɠɟɧɢɹ ɫɥɭɠɢɥɨ ɜɫɤɢɩɚɧɢɟ ɭɝɥɟɤɢɫɥɨɬɧɨ-ɜɨɞɧɨɝɨ ɮɥɸɢɞɚ. Ɇɚɥɨɬɨɧɧɚɠɧɵɟ ɤɜɚɪɰɟɜɨ-ɠɢɥɶɧɵɟ ɨɛɴɟɤɬɵ ɨɬɥɢɱɚɸɬɫɹ ɡɧɚɱɢɬɟɥɶɧɨ ɛɨɥɟɟ ɜɵɫɨɤɨɣ ɬɟɦɩɟɪɚɬɭɪɨɣ ɷɬɨɝɨ ɩɪɨɰɟɫɫɚ, ɱɬɨ ɭɤɚɡɵɜɚɟɬ ɧɚ ɨɬɧɨɫɢɬɟɥɶɧɨ ɧɢɡɤɨɟ ɞɚɜɥɟɧɢɟ ɜ ɪɭɞɨɨɛɪɚɡɭɸɳɟɣ ɫɢɫɬɟɦɟ. ɋ ɞɚɧɧɵɦ ɜɵɜɨɞɨɦ ɫɨɝɥɚɫɭɸɬɫɹ ɨɰɟɧɤɢ ɞɚɜɥɟɧɢɹ, ɫɞɟɥɚɧɧɵɟ ɩɨ ɩɥɨɬɧɨɫɬɢ ɝɚɡɨɜɵɯ ɜɤɥɸɱɟɧɢɣ (ɫɦ. ɬɚɛɥ. 2). ɉɨɞɨɛɧɚɹ ɫɜɹɡɶ ɦɨɪɮɨɥɨɝɢɢ ɪɭɞɧɵɯ ɬɟɥ ɫ ɝɥɭɛɢɧɧɨɫɬɶɸ ɦɢɧɟɪɚɥɨɨɛɪɚɡɨɜɚɧɢɹ ɦɨɠɟɬ ɛɵɬɶ ɨɛɭɫɥɨɜɥɟɧɚ ɨɫɨɛɟɧɧɨɫɬɹɦɢ ɪɚɡɜɢɬɢɹ ɪɭɞɨɜɦɟɳɚɸɳɢɯ ɫɬɪɭɤɬɭɪ: ɮɨɪɦɢɪɨɜɚɧɢɟɦ ɨɛɴɟɦɧɨɣ ɩɪɨɠɢɥɤɨɜɨ-ɜɤɪɚɩɥɟɧɧɨɣ ɦɢɧɟɪɚɥɢɡɚɰɢɢ ɜ ɫɜɹɡɢ ɫ ɦɟɥɤɨɣ ɬɪɟɳɢɧɨɜɚɬɨɫɬɶɸ ɜ ɭɫɥɨɜɢɹɯ ɜɵɫɨɤɨɝɨ ɞɚɜɥɟɧɢɹ ɢ ɨɬɞɟɥɶɧɵɯ ɤɪɭɩɧɵɯ ɪɭɞɨɜɦɟɳɚɸɳɢɯ ɬɪɟɳɢɧ – ɧɚ ɛɨɥɟɟ ɜɵɫɨɤɢɯ ɭɪɨɜɧɹɯ ɪɚɡɪɟɡɚ. Ⱦɪɭɝɢɦ ɩɪɢɡɧɚɤɨɦ ɨɬɥɢɱɢɹ ɦɚɥɨɬɨɧɧɚɠɧɵɯ ɠɢɥɶɧɵɯ ɦɟɫɬɨɪɨɠɞɟɧɢɣ ɫɥɭɠɢɬ ɲɢɪɨɤɢɣ ɞɢɚɩɚɡɨɧ ɤɨɧɰɟɧɬɪɚɰɢɣ ɢ ɬɟɦɩɟɪɚɬɭɪ ɝɨɦɨɝɟɧɢɡɚɰɢɢ ɜɨɞɧɨ-ɫɨɥɟɜɵɯ ɜɤɥɸɱɟɧɢɣ, ɤɨɬɨɪɵɣ ɨɬɪɚɠɚɟɬ ɧɟɪɚɜɧɨɦɟɪɧɨɫɬɶ ɪɚɫɩɪɟɞɟɥɟɧɢɹ ɝɚɡɨɜ ɢ ɫɨɥɟɣ ɜ ɪɭɞɨɨɛɪɚɡɭɸɳɟɣ ɫɢɫɬɟɦɟ. Ɍɚɤɚɹ ɩɪɨɫɬɪɚɧɫɬɜɟɧɧɚɹ ɞɢɮɮɟɪɟɧɰɢɚɰɢɹ ɫɨɫɬɚɜɚ ɮɥɸɢɞɧɵɯ ɩɨɬɨɤɨɜ, ɨɱɟɜɢɞɧɨ, ɩɪɨɹɜɢɥɚɫɶ ɢ ɜ ɪɚɫɩɪɟɞɟɥɟɧɢɢ ɡɨɥɨɬɚ ɜ ɨɛɴɟɦɟ ɦɟɫɬɨɪɨɠɞɟɧɢɣ. ȼɵɹɜɥɟɧɧɵɟ ɡɚɤɨɧɨɦɟɪɧɨɫɬɢ ɩɨɡɜɨɥɹɸɬ ɷɮɮɟɤɬɢɜɧɨ ɢɫɩɨɥɶɡɨɜɚɬɶ ɯɚɪɚɤɬɟɪɢɫɬɢɤɢ ɮɥɸɢɞɧɵɯ ɜɤɥɸɱɟɧɢɣ ɤɚɤ ɤɪɢɬɟɪɢɢ ɩɪɨɝɧɨɡɚ ɬɢɩɚ ɡɨɥɨɬɨɣ ɦɢɧɟɪɚɥɢɡɚɰɢɢ ɩɨ ɮɪɚɝɦɟɧɬɚɦ ɤɜɚɪɰɟɜɵɯ ɠɢɥ, ɨɛɧɚɪɭɠɟɧɧɵɯ, ɧɚɩɪɢɦɟɪ, ɜ ɪɨɫɫɵɩɹɯ ɡɨɥɨɬɚ. Ʌɢɬɟɪɚɬɭɪɚ: Bakker R. J. Package FLUIDS 1. Computer programs for analysis of fluid inclusions data and for modeling bulk fluid properties // Chemical Geology. 2003. V. 194. P. 3−23. Thiery R., Kerkhof A.M, and Dubessy J. ȞX properties of CH4-CO2 and CO2-N2 fluid inclusions: modeling for T < 31 ºC and P < 400 bars // Europ. J. Mineral. 1994. ʋ6. P. 753−771. Darling R.S. An extended equation to calculate NaCl contents from final clathrate melting temperatures in H2O-CO2-NaCl fluid inclusions: implications for PT-isochors location // Geochim. et Cosmochim. Acta. 1991. V. 55. P. 3869−3871. 127
