Pradyut Phukon , Amar Agarwal , Bruno Daniel Leite Mendes , Agnes Kontny , Gaurav Joshi
{"title":"Changes in thermomagnetic and X-ray diffraction properties of Asby dolerite with distance from the Lockne impact structure, Sweden","authors":"Pradyut Phukon , Amar Agarwal , Bruno Daniel Leite Mendes , Agnes Kontny , Gaurav Joshi","doi":"10.1016/j.pepi.2024.107145","DOIUrl":null,"url":null,"abstract":"<div><p><span>The Lockne impact structure in Sweden formed due to a meteorite impact<span><span> into the Proterozoic basement rocks in the Ordovician. The dykes of Asby </span>dolerite are part of the target basement and are located outside the crater rim. We investigated the variation in thermomagnetic properties and X-ray diffraction (XRD) spectra of Asby dolerite with distance from the crater centre to find evidence of a potential low shock overprint. Ti-poor, (Ti)-magnetite with dominantly pseudo-single domain behaviour is the main magnetic carrier in the studied samples. Towards the centre of the crater, the Verwey transition temperature (T</span></span><sub>v</sub><span>) and Curie temperature (T</span><sub>c</sub>) decrease, whereas alteration indices increase systematically. Higher alteration indices and lower T<sub>v</sub><span> near the crater centre may be owed to more intense fracturing of the silicate minerals<span> which facilitated low-temperature oxidation of (Ti)-magnetite and alteration of mafic dykes by improving fluid circulation in a network of fractures in the silicate minerals. Higher deformation near the crater centre is supported by our XRD results, as the peak position (2θ value) of plagioclase (040), pyroxene </span></span><span><math><mo>(</mo><mover><mn>3</mn><mo>¯</mo></mover><mn>11</mn></math></span>) and magnetite (311) peaks decrease, while the width of the plagioclase (040) and pyroxene <span><math><mo>(</mo><mover><mn>3</mn><mo>¯</mo></mover><mn>11</mn></math></span><span>) peaks increase towards the centre. This study shows that changes in thermomagnetic properties and lattice parameters of magnetite are a powerful tool to characterise low shock pressure deformation in impacted target rocks.</span></p></div>","PeriodicalId":54614,"journal":{"name":"Physics of the Earth and Planetary Interiors","volume":"348 ","pages":"Article 107145"},"PeriodicalIF":2.4000,"publicationDate":"2024-01-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics of the Earth and Planetary Interiors","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0031920124000037","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
The Lockne impact structure in Sweden formed due to a meteorite impact into the Proterozoic basement rocks in the Ordovician. The dykes of Asby dolerite are part of the target basement and are located outside the crater rim. We investigated the variation in thermomagnetic properties and X-ray diffraction (XRD) spectra of Asby dolerite with distance from the crater centre to find evidence of a potential low shock overprint. Ti-poor, (Ti)-magnetite with dominantly pseudo-single domain behaviour is the main magnetic carrier in the studied samples. Towards the centre of the crater, the Verwey transition temperature (Tv) and Curie temperature (Tc) decrease, whereas alteration indices increase systematically. Higher alteration indices and lower Tv near the crater centre may be owed to more intense fracturing of the silicate minerals which facilitated low-temperature oxidation of (Ti)-magnetite and alteration of mafic dykes by improving fluid circulation in a network of fractures in the silicate minerals. Higher deformation near the crater centre is supported by our XRD results, as the peak position (2θ value) of plagioclase (040), pyroxene ) and magnetite (311) peaks decrease, while the width of the plagioclase (040) and pyroxene ) peaks increase towards the centre. This study shows that changes in thermomagnetic properties and lattice parameters of magnetite are a powerful tool to characterise low shock pressure deformation in impacted target rocks.
期刊介绍:
Launched in 1968 to fill the need for an international journal in the field of planetary physics, geodesy and geophysics, Physics of the Earth and Planetary Interiors has now grown to become important reading matter for all geophysicists. It is the only journal to be entirely devoted to the physical and chemical processes of planetary interiors.
Original research papers, review articles, short communications and book reviews are all published on a regular basis; and from time to time special issues of the journal are devoted to the publication of the proceedings of symposia and congresses which the editors feel will be of particular interest to the reader.