The Molecular Weight Distribution of Occluded Hydrocarbon Gases in the Khibiny Nepheline–Syenite Massif (Kola Peninsula, NW Russia) in Relation to the Problem of Their Origin

The origin of hydrogen–hydrocarbon gases present in the rocks of the Khibiny massif in unusually high concentrations has been the subject of many years of discussion. To assess the role of potential mechanisms and relative time of formation of gases occluded in inclusions in minerals, the molecular...

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Published in:Geosciences
Main Authors: Valentin A. Nivin, Vyacheslav V. Pukha, Olga D. Mokrushina, Julia A. Mikhailova
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/geosciences12110416
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author Valentin A. Nivin
Vyacheslav V. Pukha
Olga D. Mokrushina
Julia A. Mikhailova
author_facet Valentin A. Nivin
Vyacheslav V. Pukha
Olga D. Mokrushina
Julia A. Mikhailova
author_sort Valentin A. Nivin
collection MDPI Open Access Publishing
container_issue 11
container_start_page 416
container_title Geosciences
container_volume 12
description The origin of hydrogen–hydrocarbon gases present in the rocks of the Khibiny massif in unusually high concentrations has been the subject of many years of discussion. To assess the role of potential mechanisms and relative time of formation of gases occluded in inclusions in minerals, the molecular weight distribution of C1–C5 alkanes in the main rock types of the Khibiny massif was studied. For this purpose, the occluded gases were extracted from rocks by mechanical grinding and their composition was analyzed on a gas chromatograph. It is established that the molecular weight distribution of occluded hydrocarbon gases in the Khibiny massif corresponds to the classical Anderson–Schulz–Flory distribution. In addition, the slopes of the linear relationships are relatively steep. This indicates a predominantly abiogenic origin of the occluded gases of the Khibiny massif. At the same time, a small proportion of biogenic hydrocarbons is present and is associated with the influence of meteoric waters. It was also found that in the Khibiny massif, the proportion of relatively high-temperature gases decreases towards the Main foidolite Ring in the following sequence: foyaite and khibinite–trachytoid khibinite–rischorrite and lyavochorrite–foidolites and apatite–nepheline ores. In the same sequence, an increase in the proportion of heavy hydrocarbons and the increasing role of oxidation and condensation reactions in the transformation of hydrocarbons occurs.
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https://dx.doi.org/10.3390/geosciences12110416
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spelling ftmdpi:oai:mdpi.com:/2076-3263/12/11/416/ 2025-01-16T22:55:47+00:00 The Molecular Weight Distribution of Occluded Hydrocarbon Gases in the Khibiny Nepheline–Syenite Massif (Kola Peninsula, NW Russia) in Relation to the Problem of Their Origin Valentin A. Nivin Vyacheslav V. Pukha Olga D. Mokrushina Julia A. Mikhailova agris 2022-11-11 application/pdf https://doi.org/10.3390/geosciences12110416 EN eng Multidisciplinary Digital Publishing Institute Geochemistry https://dx.doi.org/10.3390/geosciences12110416 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 12; Issue 11; Pages: 416 abiogenic hydrocarbon gases occluded gases molecular weight distribution hydrogen nepheline syenites foidolites fluid inclusions Text 2022 ftmdpi https://doi.org/10.3390/geosciences12110416 2023-08-01T07:18:28Z The origin of hydrogen–hydrocarbon gases present in the rocks of the Khibiny massif in unusually high concentrations has been the subject of many years of discussion. To assess the role of potential mechanisms and relative time of formation of gases occluded in inclusions in minerals, the molecular weight distribution of C1–C5 alkanes in the main rock types of the Khibiny massif was studied. For this purpose, the occluded gases were extracted from rocks by mechanical grinding and their composition was analyzed on a gas chromatograph. It is established that the molecular weight distribution of occluded hydrocarbon gases in the Khibiny massif corresponds to the classical Anderson–Schulz–Flory distribution. In addition, the slopes of the linear relationships are relatively steep. This indicates a predominantly abiogenic origin of the occluded gases of the Khibiny massif. At the same time, a small proportion of biogenic hydrocarbons is present and is associated with the influence of meteoric waters. It was also found that in the Khibiny massif, the proportion of relatively high-temperature gases decreases towards the Main foidolite Ring in the following sequence: foyaite and khibinite–trachytoid khibinite–rischorrite and lyavochorrite–foidolites and apatite–nepheline ores. In the same sequence, an increase in the proportion of heavy hydrocarbons and the increasing role of oxidation and condensation reactions in the transformation of hydrocarbons occurs. Text kola peninsula MDPI Open Access Publishing Khibiny ENVELOPE(33.210,33.210,67.679,67.679) Kola Peninsula Geosciences 12 11 416
spellingShingle abiogenic hydrocarbon gases
occluded gases
molecular weight distribution
hydrogen
nepheline syenites
foidolites
fluid inclusions
Valentin A. Nivin
Vyacheslav V. Pukha
Olga D. Mokrushina
Julia A. Mikhailova
The Molecular Weight Distribution of Occluded Hydrocarbon Gases in the Khibiny Nepheline–Syenite Massif (Kola Peninsula, NW Russia) in Relation to the Problem of Their Origin
title The Molecular Weight Distribution of Occluded Hydrocarbon Gases in the Khibiny Nepheline–Syenite Massif (Kola Peninsula, NW Russia) in Relation to the Problem of Their Origin
title_full The Molecular Weight Distribution of Occluded Hydrocarbon Gases in the Khibiny Nepheline–Syenite Massif (Kola Peninsula, NW Russia) in Relation to the Problem of Their Origin
title_fullStr The Molecular Weight Distribution of Occluded Hydrocarbon Gases in the Khibiny Nepheline–Syenite Massif (Kola Peninsula, NW Russia) in Relation to the Problem of Their Origin
title_full_unstemmed The Molecular Weight Distribution of Occluded Hydrocarbon Gases in the Khibiny Nepheline–Syenite Massif (Kola Peninsula, NW Russia) in Relation to the Problem of Their Origin
title_short The Molecular Weight Distribution of Occluded Hydrocarbon Gases in the Khibiny Nepheline–Syenite Massif (Kola Peninsula, NW Russia) in Relation to the Problem of Their Origin
title_sort molecular weight distribution of occluded hydrocarbon gases in the khibiny nepheline–syenite massif (kola peninsula, nw russia) in relation to the problem of their origin
topic abiogenic hydrocarbon gases
occluded gases
molecular weight distribution
hydrogen
nepheline syenites
foidolites
fluid inclusions
topic_facet abiogenic hydrocarbon gases
occluded gases
molecular weight distribution
hydrogen
nepheline syenites
foidolites
fluid inclusions
url https://doi.org/10.3390/geosciences12110416