Lead isotopic systematics of massive sulphide deposits in the Urals: Applications for geodynamic setting and metal sources

Tessalina, Svetlana; Herrington, Richard; Taylor, Rex N.; Sundblad, Krister; Масленников, В. В.; Orgeval, J.-J.

doi:10.1016/j.oregeorev.2015.06.016

Cited by 30 publications

(6 citation statements)

References 47 publications

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“…2015). In addition, Pb isotopic analysis is useful for constraining the origin of metals within 105 mineral deposits (Zhou et al, 2001;Cunha et al, 2007;Zeng et al, 2014;Tessalina et al, 2016). 106…”

Section: Introduction 51mentioning

confidence: 99%

S, Pb, and Sr isotope geochemistry and genesis of Pb–Zn mineralization in the Huangshaping polymetallic ore deposit of southern Hunan Province, China

Ding

et al. 2016

Ore Geology Reviews

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The Huangshaping Pb-Zn-W-Mo polymetallic deposit, located in southern Hunan 9 Province, China, is one of the largest deposits in the region and is unique for its metals 10 combination of Pb-Zn-W-Mo and the occurrence of significant reserves of all these metals. The 11 deposit contains disseminated scheelite and molybdenite within a skarn zone located between 12 Jurassic granitoids and Carboniferous sedimentary carbonate, and sulfide ores located within distal 13 carbonate-hosted stratiform orebodies. The metals and fluids that formed the W-Mo 14 mineralization were derived from granitoids, as indicated by their close spatial and temporal 15 relationships. However, the source of the Pb-Zn mineralization in this deposit remains 16 controversial. 17 Here, we present new sulfur, lead, and strontium isotope data of sulfide minerals (pyrrhotite, 18 sphalerite, galena, and pyrite) from the Pb-Zn mineralization within the deposit, and these data are 19 compared with those of granitoids and sedimentary carbonate in the Huangshaping deposit, 20 thereby providing insights into the genesis of the Pb-Zn mineralization. These data indicate that 21 the sulfide ores from deep levels in the Huangshaping deposit have lower and more consistent 22

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Section: Introduction 51mentioning

confidence: 99%

S, Pb, and Sr isotope geochemistry and genesis of Pb–Zn mineralization in the Huangshaping polymetallic ore deposit of southern Hunan Province, China

Ding

et al. 2016

Ore Geology Reviews

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“…Several reviews describe the geological setting of the Urals VHMS deposits (hereafter, deposits) [17,19,32,[35][36][37][38][39][40][41][42][43][44][45]. The deposits studied were formed in a range of tectonic settings, including marginal sea (Yaman-Kasy), fore-arc basin (Dergamysh), bimodal mafic (Yubileynoe, Molodezhnoe), and felsic (Saf'yanovskoe deposit) intra-arc basin settings, see Figure 1.…”

Section: Geological Setting and Types Of The Deposits Studiedmentioning

confidence: 99%

Mineralogical Features of Ore Diagenites in the Urals Massive Sulfide Deposits, Russia

et al. 2019

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In weakly metamorphosed massive sulfide deposits of the Urals (Dergamysh, Yubileynoe, Yaman-Kasy, Molodezhnoe, Valentorskoe, Aleksandrinskoe, Saf’yanovskoe), banded sulfides (ore diagenites) are recognized as the products of seafloor supergene alteration (halmyrolysis) of fine-clastic sulfide sediments and further diagenesis leading to the formation of authigenic mineralization. The ore diagenites are subdivided into pyrrhotite-, chalcopyrite-, bornite-, sphalerite-, barite- and hematite-rich types. The relative contents of sphalerite-, bornite- and barite-rich facies increases in the progression from ultramafic (=Atlantic) to bimodal mafic (=Uralian) and bimodal felsic (=Baymak and Rudny Altay) types of massive sulfide deposits. The ore diagenites have lost primary features within the ore clasts and dominantly exhibit replacement and neo-formed nodular microtextures. The evolution of the mineralogy is dependent on the original primary composition, sizes and proportions of the hydrothermal ore clasts mixed with lithic serpentinite and hyaloclastic volcanic fragments together with carbonaceous and calcareous fragments. Each type of ore diagenite is characterized by specific rare mineral assemblages: Cu–Co–Ni sulfides are common in pyrrhotite-rich diagenites; tellurides and selenides in chalcopyrite-rich diagenites; minerals of the germanite group and Cu–Ag and Cu–Sn sulfides in bornite-rich diagenites; abundant galena and sulfosalts in barite- and sphalerite-rich diagenites and diverse tellurides characterize hematite-rich diagenites. Native gold in variable amounts is typical of all types of diagenites.

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“…Proprioceptive sense measurements were taken by using an isokinetic dynamometer of Pro-Kin, Technology, Dalmine, Italy brand (20 Hz sampling rate, sensitivity 0.1°, product type:PK252). Proprioceptive Sense Test was carried out by the selection of Multiaxial Proprioceptive Assessment Module with a proven validity and reliability (Tessalina et. al, 2016;Wang et.…”

Section: Proprioceptive Sense Measurementsmentioning

confidence: 99%

Effect of Maximal Anaerobic Loading on Lower Extremity Proprioceptive Sense in Soccer Players

Göktepe

Çakır²,

Göktepe³

et al. 2019

JETS

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This study was carried out to determine the effect of lower extremity muscle fatigue on proprioceptive sense in soccer players. 26 male soccer players who play licensed soccer in the amateur soccer teams of the Ağrı province and who was not injured in the past year (Age 20,03±3,38, weight 65,69±10,66, height 176,61±8,72) participated in the study voluntarily. The lactic acid concentration of the participants at rest and their proprioceptive sense measurements were determined by standardized methods and materials. Then, Wingate test was applied to the participants. The lactic acid concentration and proprioceptive sense measurements were repeated at the end of the test. The analysis of the collected data was carried out through the SPSS 22 program. Shapiro-Wilks test was conducted for normality distribution. Independent-Samples t-test was carried out in the comparison of test and control groups and Paired-Samples t-Test was utilized in the comparison of differences between pretest and posttest means. It was concluded that lower extremity fatigue in soccer players has a negative effect on lower extremity proprioceptive sense (p<0.05).

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Lead isotopic systematics of massive sulphide deposits in the Urals: Applications for geodynamic setting and metal sources

Cited by 30 publications

References 47 publications

S, Pb, and Sr isotope geochemistry and genesis of Pb–Zn mineralization in the Huangshaping polymetallic ore deposit of southern Hunan Province, China

S, Pb, and Sr isotope geochemistry and genesis of Pb–Zn mineralization in the Huangshaping polymetallic ore deposit of southern Hunan Province, China

Mineralogical Features of Ore Diagenites in the Urals Massive Sulfide Deposits, Russia

Effect of Maximal Anaerobic Loading on Lower Extremity Proprioceptive Sense in Soccer Players

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