Infrared spectra study of the Moslavacka Gora (Croatia) tourmalines O-H stretching region: Inference of fluid involvement in the late cretaceous igneous evolution of a complex Adria-Europe convergence zone

Q4 Earth and Planetary Sciences Geoloski Anali Balkanskoga Poluostrva Pub Date : 2023-01-01 DOI:10.2298/gabp230301003b
Drazen Balen, Zorica Petrinec
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引用次数: 1

Abstract

Infrared spectra (IR) in the O-H stretching region were recorded for natural tourmalines from the magmatic and magmatic-hydrothermal systems of Moslavacka Gora (Croatia). Samples of disseminated tourmaline (schorl) representing magmatic products were collected from leucogranite. Nodular tourmaline (intermediate members of the schorl-dravite series) from twomica granite represents a magmatic-hydrothermal mineral related to the final stage of granite crystallization. IR spectra of the typically disseminated tourmaline show four sharp O-H stretching bands: 3643, 3633, 3550, and 3484 cm?1, while typical nodular tourmaline shows spectra with asymmetric and relatively broad O-H stretching bands on 3635 and 3554 cm?1 with shoulders at the higher and lower wavenumber side. The broadening in the lower wavenumber region of nodular tourmaline compared to disseminated tourmaline indicates a higher water content in the nodular type. At the same time, the observed shifts between the corresponding bands can be explained by the shortening of the O-H1 and O-H3 distances, which can be attributed to different genetic and/or evolutionary processes. According to the models applicable to the Moslavacka Gora, disseminated tourmaline from the leucogranite can be considered a typical magmatic (pegmatitic) product and a standard accessory phase of the leucogranite. The origin of nodular tourmaline, which was the last mineral to crystallize in the evolved Late Cretaceous granitic system of Moslavacka Gora, is attributed to the interaction of a fluid phase from the residual granitic melt with the fluid originating from the wall-rock in the low-pressure crustal setting, which was accompanied by relatively rapid cooling. This interaction resulted in an increased dravite content of the nodular tourmaline and is reflected in the observed IR spectral features.
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Moslavacka Gora (Croatia)电气石O-H伸展区的红外光谱研究:流体参与晚白垩世复杂亚德里亚-欧洲辐合带火成岩演化的推断
本文记录了克罗地亚Moslavacka Gora岩浆和岩浆-热液系统中天然电气石的O-H伸展区红外光谱。从浅花岗岩中采集了代表岩浆产物的浸染电气石样品。两洲花岗岩中的结核状电气石(榴辉岩系列的中间成员)是一种岩浆热液矿物,与花岗岩结晶的最后阶段有关。典型浸染电气石的红外光谱显示出四个明显的O-H拉伸带:3643、3633、3550和3484 cm?1 .典型的结节状碧玺在3635和3554 cm?1在较高和较低的波数侧肩部。结核型碧玺较浸染型碧玺低波数区变宽,表明结核型碧玺含水量较高。同时,观测到的相应波段之间的位移可以解释为O-H1和O-H3距离的缩短,这可以归因于不同的遗传和/或进化过程。根据适用于莫斯拉瓦卡戈拉地区的模型,该浅色花岗岩中的浸染电气石可视为典型的岩浆(伟晶岩)产物,是浅色花岗岩的标准附属相。结核状电气石是演化的晚白垩世莫斯拉夫瓦卡戈拉花岗岩体系中最后结晶的矿物,其成因是低压地壳环境下残余花岗岩熔体的流体相与围岩流体的相互作用,并伴有相对快速的冷却过程。这种相互作用导致了瘤状电气石中钛矿含量的增加,并反映在观察到的红外光谱特征中。
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来源期刊
Geoloski Anali Balkanskoga Poluostrva
Geoloski Anali Balkanskoga Poluostrva Earth and Planetary Sciences-Geophysics
CiteScore
1.40
自引率
0.00%
发文量
4
审稿时长
24 weeks
期刊最新文献
Understanding geodynamics of the long-lasting Adria-Europe convergence: new constraints from the central balkans Infrared spectra study of the Moslavacka Gora (Croatia) tourmalines O-H stretching region: Inference of fluid involvement in the late cretaceous igneous evolution of a complex Adria-Europe convergence zone From shallow-water carbonate ramp to hemipelagic deep-marine carbonate deposition: Part 1. General characteristics, microfacies and depositional history of the Middle to Late Anisian Bulog sedimentary succession in the Inner Dinarides (SW Serbia) Evolution of the southeastern part of the Pannonian Basin and its implications From shallow-water carbonate ramp to hemipelagic deep-marine carbonate deposition: Part 2. Sirogojno (Klisura quarry) - the reference section of the Middle to Late Anisian Bulog sedimentary succession in the Inner Dinarides (SW Serbia)
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