Rare earth elements, yttrium and Pb isotope ratios in thermal spring and well waters of West Anatolia, Turkey: a hydrochemical study of their origin

Möller, P.; Dulski, Peter; Savascin, Y; Conrad, Mark E.

doi:10.1016/j.chemgeo.2004.01.009

Cited by 65 publications

(19 citation statements)

References 33 publications

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“…In general, Eu anomaly is strongly lithology-dependent (Tricca et al 1999;Möller et al 2004). Thus, waters originating from source rocks with positive Eu anomalies have similarly positive anomalies whereas waters from source rocks with negative anomalies have also negative Eu anomalies.…”

Section: Average Ree Pattern Of Dissolved Loadmentioning

confidence: 98%

Rare Earth Element Patterns in the Karst Terrains of Guizhou Province, China: Implication for Water/Particle Interaction

Han

Tang

et al. 2009

Aquat Geochem

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The authors determine the concentrations of dissolved (\0.22 lm) rare earth elements (REE) and suspended particulate matter (SPM) of typical karst rivers in Guizhou Province, China during the high-flow period. The concentrations of acid-soluble REE extracted from SPM using diluted hydrochloric acid are also obtained to investigate water/ particle interaction in the river water. The dissolved REE contents in the river water are extremely low in the rivers of the study. The dissolved REE distribution patterns normalized by the Post Archean Australia Shale (PAAS) in the karst rivers are not flat, show slight enrichment of heavy REE to light REE, and also have significant negative Ce and Eu anomalies. The acid-soluble REE appears to have similar distribution patterns as characterized by MREE enrichment and slight LREE depletion, with unremarkable Ce and Eu anomalies. The PAAS-normalized REE distribution patterns of SPM are flat with negative Eu anomalies. The contents and distribution patterns of REE in the SPM are closely related to the lithological character of the source rocks. The SPM contains almost all the REE produced in the process of surficial weathering. This demonstrates that particle-hosted REE are the most important form of REE occurrence. REE fractionation, which takes place during weathering and transport, leads to an obvious HREE enrichment in the dissolved loads relative to the SPM. Y/Ho ratio can be used to shed light on REE behaviors during water/particle interaction.

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Section: Average Ree Pattern Of Dissolved Loadmentioning

confidence: 98%

Rare Earth Element Patterns in the Karst Terrains of Guizhou Province, China: Implication for Water/Particle Interaction

Han

Tang

et al. 2009

Aquat Geochem

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“…The easily accessible REEY content was determined for a number of granites, gneisses and low-grade metasedimentary samples using a cation exchange resin to extract REEY at 70°C and pH~3 (e.g., Möller et al, 1997aMöller et al, , 1997bMöller et al, , 2003Möller et al, , 2004. This generally resulted in upward-convex crust-normalized REEY patterns (Fig.…”

Section: Reey Sourcing During Fluid-rock Interactionsmentioning

confidence: 99%

Unraveling rare earth element signatures in hydrothermal carbonate minerals using a source–sink system

Debruyne

Hulsbosch

Muchez

2016

Ore Geology Reviews

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“…Geothermal fluids from Larderello‐Travale/Italy (Möller et al. 2003b), Kizildere/Turkey (Möller et al. 2004).…”

Section: Rare Earth Elements and Yttriummentioning

confidence: 99%

“…2B). Three types of REY patterns can be distinguished: (i) patterns with strongly negative Eu anomalies characterizing waters from granites (Möller 2002; Möller et al. 2003a, 2004), (ii) U‐shaped patterns typical for water from mafic rocks (Paces et al.…”

Section: Rare Earth Elements and Yttriummentioning

confidence: 99%

Main and trace elements in KTB‐VB fluid: composition and hints to its origin

Möller¹,

Woith²,

Dulski³

et al. 2005

Geofluids

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The pilot hole (VB) of the German Continental Deep Drilling Program (KTB) was drilled to a depth of 4000 m, where large amounts of free fluids were met. The KTB-VB 4000 m fluid can be related to either Mesozoic seawater or formation water from Permo-Carboniferous sedimentary rocks of the Weiden embayment. During the Upper Cretaceous uplift of the Bohemian Massif both fluids could have passed organic-rich Triassic to Carboniferous formations of the Weiden embayment before invading the uplifted and fractured basement rocks of Devonian amphibolites and metagabbros, where the chemical composition of the fluids was changed by albitization, adularization, and chloritization. Results of chemical mass balances for both sources are presented. In order to concentrate the formation water from the Weiden embayment significant amphibolitization has to be assumed. During a 1-year pumping test the chemical composition of the 4000 m fluids remained constant. The accuracy of chemical analyses is critically reviewed. An improved preconcentration method of rare earth elements and yttrium in high-Ca-bearing saline fluids is described.

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Rare earth elements, yttrium and Pb isotope ratios in thermal spring and well waters of West Anatolia, Turkey: a hydrochemical study of their origin

Cited by 65 publications

References 33 publications

Rare Earth Element Patterns in the Karst Terrains of Guizhou Province, China: Implication for Water/Particle Interaction

Rare Earth Element Patterns in the Karst Terrains of Guizhou Province, China: Implication for Water/Particle Interaction

Unraveling rare earth element signatures in hydrothermal carbonate minerals using a source–sink system

Main and trace elements in KTB‐VB fluid: composition and hints to its origin

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