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Pauzhetka Field

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Journal Article
Published: 01 September 2020
Russ. Geol. Geophys. (2020) 61 (9): 976–993.
... geothermal deposit (southern Kamchatka). An isometric concentric zonal structure has been identified within the temperature, geoelectric, magnetic, and gravimetric fields. It spatially correlates with an elevated tectonic block previously detected in the area of the Upper Pauzhetka thermal field. The central...
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Journal Article
Published: 01 November 2019
Russ. Geol. Geophys. (2019) 60 (11): 1267–1277.
... of the craters of active volcanoes (Ebeko and Mutnovskii). Mud water pools of the craters contain mainly sulfur, opal, and α-quartz. An assemblage of kaolinite, opal, alunite group minerals (in small amounts), and goethite forms in mud water pools with pH = 2–3 in the thermal fields of the Pauzhetka–Kambal’nyi...
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A fragment of the map of the anomalous magnetic <b>field</b> of the <b>Pauzhetka</b> geot...
Published: 01 September 2020
Fig. 7. A fragment of the map of the anomalous magnetic field of the Pauzhetka geothermal deposit (from ( Nuzhdaev et al., 2014 )): distribution of Δ T а values on the area ( a ) and along the profile ( b ).
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Diverse thermal manifestations of the <b>Pauzhetka</b>–Kambal’nyi–Koshelevskii reg...
Published: 01 November 2019
), Upper Pauzhetka thermal fields ( 4 , 5 , 8 ), and Lower Koshelevskii thermal anomaly ( 6 , 7 ).
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A conceptual model for the structure of the Upper <b>Pauzhetka</b> t&#x2F;f of the Pauz...
Published: 01 September 2020
Fig. 10. A conceptual model for the structure of the Upper Pauzhetka t/f of the Pauzhetka hydrothermal system (Photo by M.S. Chernov). 1 , the foundation of the structure: volcanomictic sandstones; 2 , water-bearing strata of rocks: lower, agglomerate tuffs, upper, coarse-grained tuffs; 3
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The diagram of distribution of the self-potential <b>field</b> values in the Upper...
Published: 01 September 2020
Fig. 6. The diagram of distribution of the self-potential field values in the Upper Pauzhetka t/p: a , on the area, b , along the profile.
Journal Article
Published: 01 October 2018
Mineralogical Magazine (2018) 82 (5): 1057–1077.
...) geothermal field, Kambalny volcanic ridge, Southern Kamchatka, Russia. Ammoniovoltaite forms at ~100°C around geothermal gas/steam vents in association with alunogen, tschermigite and pyrite. Crystals of ammoniovoltaite have euhedral habit, are up to 50 µm in size and grow on alunogen plates. Ammoniovoltaite...
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Schematic geological map of the Pauzhetsky hydrothermal system (from  Rycha...
Published: 01 September 2020
and andesibasalts of Middle Quaternary Age; 4 , alluvial boulder-pebble deposits; 5 , ring tectonic faults that delineate elevated blocks of rocks and control the position of thermal fields; 6 , linear tectonic faults; 7 , Pauzhetka graben of upper Quaternary Age; 8 , thermal fields: 1, South Pauzhetka, 2
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Diffraction patterns of the air-dried ( a ) and glycerol-saturated ( b ) cl...
Published: 01 November 2019
Fig. 6. Diffraction patterns of the air-dried ( a ) and glycerol-saturated ( b ) clay fractions of mud water pools ( 1–4 ) and steaming ground ( 5–8 ) of the Upper Pauzhetka ( 1, 6 ), Nizhnii Koshelevskii ( 2, 3 ), and East Pauzhetka ( 5 , 7, 8 ) thermal fields; theoretical diffraction patterns
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IR spectra of clays composing the walls of steam–gas jets of the East Pauzh...
Published: 01 November 2019
Fig. 7. IR spectra of clays composing the walls of steam–gas jets of the East Pauzhetka thermal field ( 1, 2 ), North Kambal’nyi steam jets ( 3 ), and Lower Koshelevskii thermal anomaly ( 4, 5 ), in the ranges 400–1600 cm −1 (I) and 3000–4000 cm −1 (II).
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AFM images of the surface of pyrite crystals of different geneses.  a ,  b ...
Published: 01 October 2015
Fig. 5. AFM images of the surface of pyrite crystals of different geneses. a , b , Sukhoi Log; a , sample 42–54; b , sample 112p-135; c , sample VPP—low-temperature pyrite from the clays of the East Pauzhetka thermal field (Kamchatka Peninsula). Numbers show the image size.
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Geographical ( a ) and geological ( b ) maps of the southwestern part of th...
Published: 01 November 2019
, a , secondary quartzites, b , argillizites; 10 , geothermal fields: 1, first hot springs, 2, Pauzhetka hydrothermal deposit, 3, North Kambal’nyi steam jets, 4, Central Kambal’nyi, 5, South Kambal’nyi, 6, Upper Koshelevskii, 7, Lower Koshelevskii ( Rychagov et al., 2014 ; Zhitova et al., 2017 , 2018 ).
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Mapping of information derived from geophysical observations in the area of...
Published: 01 September 2020
Fig. 3. Mapping of information derived from geophysical observations in the area of the Upper Pauzhetka t/f: a , temperature survey, b , electrical prospecting, c , gravity prospecting. We used the magnetic surveys as a topographic base. 1 , averaged contour of the thermal field drawn along
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Geographical (upper) and geological (lower) maps of the south-western part ...
Published: 01 October 2018
Fig. 1. Geographical (upper) and geological (lower) maps of the south-western part of Kamchaka Peninsula (Rychagov et al ., 2014 ). Key: (1) 1ava-pyroclastic sediments of Neogene age; (2) volcanogenic-sedimentary rocks (tuffites) of Pauzhetka suite; (3) ignimbrites; (4) lava complexes
Journal Article
Published: 01 October 2015
Russ. Geol. Geophys. (2015) 56 (10): 1394–1413.
...Fig. 5. AFM images of the surface of pyrite crystals of different geneses. a , b , Sukhoi Log; a , sample 42–54; b , sample 112p-135; c , sample VPP—low-temperature pyrite from the clays of the East Pauzhetka thermal field (Kamchatka Peninsula). Numbers show the image size. ...
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Journal Article
Published: 01 February 2020
Russ. Geol. Geophys. (2020) 61 (2): 224–233.
... – 648 . Ratnikova L.I. , 1973 . Methods for Modeling Seismic Fields in a Thin-Layered Earth [in Russian]. Nauka, Moscow . Rautian , T.G. , Khalturin , V.I. , 1978 . The use of the coda for determination of the earthquake source spectrum . Bull. Seismol. Soc. Am. 68 ( 4...
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Journal Article
Published: 01 January 2001
Reviews in Mineralogy and Geochemistry (2001) 45 (1): 305–322.
... zeolites, have been identified in the Pauzhetka geothermal area, Kamchatka (Fig. 4 , Loc. 7) ( Noboko 1976 ). Zeolites appear mainly at the periphery of the geothermal area and are zonally distributed from top to bottom as follows: authigenic mineral-free ⇒ analcime ⇒ montmorillonite ⇒ mordenite...
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Series: Special Publications of the Society of Economic Geologists, Special Publications of the Society of Economic Geologists
Published: 01 January 2005
DOI: 10.5382/SP.10.04
EISBN: 9781629490342
... Mole Ratio in Gases from Wells and Steam Vents in Some Geothermal Fields Codes (see Fig. 3 ) Geothermal system N 2 /Ar Ref. ru El Ruiz 1,680 295 1 ru El Ruiz 1.6 86 1 cf Campi Flegrei 33 738 1 kr Krafla 1.9 69 1 mt Mutnovsky 90 220 2 pz...
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