4.5 Article

3D Raman mapping combined with FIB-SEM on multiphase fluid inclusions: A tool to unravel complex phase assemblages

期刊

JOURNAL OF RAMAN SPECTROSCOPY
卷 -, 期 -, 页码 -

出版社

WILEY
DOI: 10.1002/jrs.6564

关键词

3D Raman mapping; multiphase fluid inclusions; Raman cross section; volume percentages

向作者/读者索取更多资源

In this study, high resolution 3D Raman mapping was performed on primary multiphase fluid inclusions from the Cabo Ortegal Complex in NW Spain. The study demonstrates that the optical and Raman scattering properties of phases inside the inclusions can affect the accuracy of both 2D and 3D Raman maps. By comparing 3D Raman models with submicron-scale slicing, the evaluation of Raman spectroscopy data was optimized and volume proportion calculations were provided. The results have implications for thermodynamic modeling and fluid/rock interactions.
In this study, we performed high resolution 3D Raman mapping on primary multiphase fluid inclusions from a granulite and an eclogite of the Cabo Ortegal Complex (NW Spain), the latter representing a former subduction zone environment. Several microns-sized inclusions are great targets to test the advantages and limitations of 3D Raman mapping. We show how optical and Raman scattering properties of the phases inside the inclusions can affect the veracity of both 2D and 3D Raman maps. As an independent control, 3D Raman models were compared with focused ion beam-scanning electron microscopy submicron-scale slicing of three previously 3D Raman mapped inclusions, allowing us to optimize Raman spectroscopy data evaluation and provide volume proportion calculations. We found that a non-optimized evaluation procedure might result in even an order of magnitude over- or underestimation of phase volume properties. We propose that correcting the Raman maps even with empirically determined Raman cross sections of the phases inside the inclusions can vastly improve the quality of the maps. The results provide valuable input data for thermodynamic modeling and draw implications for fluid/rock interactions.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.5
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

Article Geochemistry & Geophysics

The role of water and compression in the genesis of alkaline basalts: Inferences from the Carpathian-Pannonian region

I Kovacs, L. Patko, N. Liptai, T. P. Lange, Z. Taracsak, S. A. P. L. Cloetingh, K. Torok, E. Kiraly, D. Karatson, T. Biro, J. Kiss, Zs Palos, L. E. Aradi, Gy Falus, K. Hidas, M. Berkesi, A. Koptev, A. Novak, V Wesztergom, T. Fancsik, Cs Szabo

LITHOS (2020)

Article Geosciences, Multidisciplinary

Carbonatite and highly peralkaline nephelinite melts from Oldoinyo Lengai Volcano, Tanzania: The role of natrite-normative fluid degassing

Marta Berkesi, Eniko Bali, Robert J. Bodnar, Abel Szabo, Tibor Guzmics

GONDWANA RESEARCH (2020)

Article Geography, Physical

Effect of water on the rheology of the lithospheric mantle in young extensional basin systems as shown by xenoliths from the Carpathian-Pannonian region

Nora Liptai, Thomas P. Lange, Levente Patko, Zsanett Pinter, Marta Berkesi, Laszlo E. Aradi, Csaba Szabo, Istvan J. Kovacs

Summary: In this study, the water contents in upper mantle xenoliths in the Carpathian-Pannonian region were comprehensively examined, revealing higher water contents in Tihany xenoliths compared to Flizes-to xenoliths. Differences in water contents may be influenced by factors such as eruption age and depth of origin. Additionally, variations in effective viscosities and electrical resistivities suggest that central locations have more rigid lithospheric mantles compared to marginal locations, potentially influenced by extension-related lithospheric thinning.

GLOBAL AND PLANETARY CHANGE (2021)

Article Geochemistry & Geophysics

Characterization of the metasomatizing agent in the upper mantle beneath the northern Pannonian Basin based on Raman imaging, FIB-SEM, and LA-ICP-MS analyses of silicate melt inclusions in spinel peridotite

Nora Liptai, Marta Berkesi, Levente Patko, Robert J. Bodnar, Suzanne Y. O'Reilly, William L. Griffin, Csaba Szabo

Summary: The study analyzed silicate melt inclusions to determine the composition and evolution of metasomatic melt in the upper mantle. The trapped metasomatic melt linked to wehrlite formation was found to be enriched in iron with a trace-element pattern similar to OIB, suggesting an intraplate mafic melt with a slightly different chemistry compared to the host basalt.

AMERICAN MINERALOGIST (2021)

Article Geochemistry & Geophysics

Iron isotope and trace metal variations during mantle metasomatism: In situ study on sulfide minerals from peridotite xenoliths from Nograd-Gomor Volcanic Field (Northern Pannonian Basin)

Levente Patko, Jakub Ciazela, Laszlo Elod Aradi, Nora Liptai, Bartosz Pieterek, Marta Berkesi, Marina Lazarov, Istvan Janos Kovacs, Francois Holtz, Csaba Szabo

Summary: Sulfides from lherzolite and wehrlite xenoliths in the Nograd-Gomor Volcanic Field were studied to understand the behavior of chalcophile and siderophile elements. Significant differences were found in the composition and distribution of sulfides between the two xenolith types, suggesting enrichment of sulfides and chalcophile elements in the subcontinental lithospheric mantle due to metasomatism.

LITHOS (2021)

Article Geography, Physical

The 'pargasosphere' hypothesis: Looking at global plate tectonics from a new perspective

Istvan J. Kovacs, Nora Liptai, Alexander Koptev, Sierd A. P. L. Cloetingh, Thomas P. Lange, Liviu Matenco, Alexandru Szakacs, Mircea Radulian, Marta Berkesi, Levente Patko, Gabor Molnar, Attila Novak, Viktor Wesztergom, Csaba Szabo, Tamas Fancsik

Summary: The 'pargasosphere' hypothesis proposed by the author explains the role of MLDs in continental lithospheres and offers a mechanism for the formation of MLDs. The hypothesis also presents several empirically testable implications.

GLOBAL AND PLANETARY CHANGE (2021)

Article Geology

Abiotic passive nitrogen and methane enrichment during exhumation of subducted rocks: Primary multiphase fluid inclusions in high-pressure rocks from the Cabo Ortegal Complex, NW Spain

Tamas Spranitz, Jose Alberto Padron-Navarta, Csaba Szabo, Abel Szabo, Marta Berkesi

Summary: The primary multiphase fluid inclusions (MFI) in the Cabo Ortegal Complex (COC) in NW Spain were found to be formed under high-pressure metamorphic conditions. The mineral assemblage of MFI consists mainly of carbonates and silicates, with proportions of nitrogen, methane and carbon dioxide. Reactions between the MFI and the host minerals resulted in carbonation and hydration reactions. This study has important implications for global nitrogen and carbon cycling, as well as the supply of nitrogen and methane in subsurface-surface environments.

JOURNAL OF METAMORPHIC GEOLOGY (2022)

Article Geosciences, Multidisciplinary

Deciphering metasomatic events beneath Mindszentkalla (Bakony-Balaton Highland Volcanic Field, western Pannonian Basin) revealed by single-lithology and composite upper mantle xenoliths

Levente Patko, Zoltan Kovacs, Nora Liptai, Laszlo E. Aradi, Marta Berkesi, Jakub Ciazela, Karoly Hidas, Carlos J. Garrido, Istvan J. Kovacs, Csaba Szabo

Summary: The single-lithology and composite xenoliths from Mindszentkalla provide insights into the geochemical evolution of the subcontinental lithospheric mantle. These xenoliths show evidence of at least two metasomatic events, with the first event leading to orthopyroxene enrichment and the formation of harzburgites. The different domains of the composite xenoliths likely represent reaction products of variably evolved basaltic melts. The formation of these xenoliths is likely linked to past subduction of oceanic crust and plate extrusion.

FRONTIERS IN EARTH SCIENCE (2022)

Article Geosciences, Multidisciplinary

Reconstruction of magma chamber processes preserved in olivine-phlogopite micro-ijolites from the Oldoinyo Lengai, Tanzania

Noemi Halasz, Marta Berkesi, Tivadar M. Toth, Roger H. Mitchell, Ralf Milke, Tibor Guzmics

Summary: A detailed petrographic and mineralogical investigation of olivine-phlogopite micro-ijolite xenoliths from Oldoinyo Lengai, Tanzania reveals their complex evolutionary history and diverse textural features. The xenoliths show crystallization temperatures ranging from 1070-970 degrees C to 850-700 degrees C, controlled by perovskite-titanite equilibria under plutonic pressures. The presence of double coronas and compositional zonation in the xenoliths suggests early magma chamber processes and multiple magma injections followed by cooling periods. The study provides insights into the origin and formation processes of these micro-ijolite xenoliths.

JOURNAL OF AFRICAN EARTH SCIENCES (2023)

Article Geochemistry & Geophysics

Carbonatite formation in continental settings via high pressure - high temperature liquid immiscibility

Marta Berkesi, Justine L. Myovela, Gregory M. Yaxley, Tibor Guzmics

Summary: The study compares high temperature silicate-carbonatite immiscible melts with silica-undersaturated volcanic rocks from continental settings to understand the formation of calcite carbonatite rocks. Melt inclusions from the Kerimasi volcano in the East African Rift System show early formation of the rock and entrapment of melts at high temperatures and pressures. The presence of immiscible mafic-melilitite and Ca-Na-K-carbonatite melts suggests a continental rift setting and the crystallization of calcite carbonatite rocks.

GEOCHIMICA ET COSMOCHIMICA ACTA (2023)

Article Geochemistry & Geophysics

Estimation of P-T entrapment conditions of a subduction fluid using elastic thermobarometry: A case study from Cabo Ortegal Complex, Spain

Tamas Spranitz, Csaba Szabo, Mattia Gilio, Matteo Alvaro, Michaela Blazekova, Patrik Konecny, Tamas Vaczi, Marta Berkesi

Summary: Fluid and mineral inclusions in metamorphic rocks play a crucial role in understanding fluid-involved processes in subduction zones. This study focuses on ultramafic granulite from the Cabo Ortegal Complex in Spain, using quartz-in-garnet and zircon-in-garnet Raman spectroscopy to determine the entrapment conditions of mineral and fluid inclusions. The findings confirm the reliability of elastic thermobarometry on mineral inclusions in determining the entrapment P-T conditions. Rating: 8 out of 10.

LITHOS (2023)

Article Geosciences, Multidisciplinary

Tectonically-determined distribution of monogenetic volcanoes in a compressive tectonic regime: An example from the Pannonian continental back-arc system (Central Europe)

Matyas Hencz, Tamas Biro, Karoly Nemeth, Kristof Porkolab, Istvan Janos Kovacs, Tamas Spranitz, Sierd Cloetingh, Csaba Szabo, Marta Berkesi

Summary: This paper presents the results of using a GIS workflow to analyze the spatial distribution and temporal evolution of volcanoes in the Mio-Pleistocene monogenetic Bakony-Balaton Highland Volcanic Field (BBHVF) in Hungary. The study reveals the importance of the pre-existing structure of the upper lithosphere in the distribution of volcanic centers. The orientation of the volcanic field is found to correspond to the orientation of faults in the region, suggesting a dominant SW-NE direction. The proximity analysis also indicates the significance of thrust faults in the clustering of the volcanoes.

JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH (2023)

暂无数据