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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Antarctica (2)
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Europe
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Alps
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Western Alps (1)
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Southern Europe
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Italy
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Ivrea-Verbano Zone (1)
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Piemonte Italy
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Ivrea Italy (1)
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South America
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Parana Basin (1)
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elements, isotopes
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carbon (1)
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igneous rocks
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igneous rocks
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volcanic rocks
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basalts (1)
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metamorphic rocks
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metamorphic rocks
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granulites
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kinzigite (1)
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metaigneous rocks
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metagabbro (1)
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mylonites
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pseudotachylite (1)
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meteorites
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meteorites
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stony irons
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mesosiderite (1)
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stony meteorites
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achondrites
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minerals
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pyroxene group
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framework silicates
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orthosilicates
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nesosilicates
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Primary terms
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Antarctica (2)
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carbon (1)
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core (1)
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crystal chemistry (1)
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crystal growth (1)
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deformation (1)
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Europe
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Alps
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Western Alps (1)
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Southern Europe
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Italy
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Ivrea-Verbano Zone (1)
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Piemonte Italy
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Ivrea Italy (1)
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faults (1)
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geochemistry (1)
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igneous rocks
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volcanic rocks
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basalts (1)
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mantle (1)
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granulites
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kinzigite (1)
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metaigneous rocks
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metagabbro (1)
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mylonites
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pseudotachylite (1)
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metamorphism (2)
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metasomatism (1)
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meteorites
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Asuka Meteorites (1)
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stony irons
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mesosiderite (1)
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stony meteorites
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achondrites
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ureilite (1)
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Yamato Meteorites (1)
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South America
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Parana Basin (1)
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Characterization of carbon phases in Yamato 74123 ureilite to constrain the meteorite shock history
ABSTRACT Constraints on impact-related hydrothermal alteration are important to enable the reconstruction of the possible processes affecting the surface of other terrestrial planets, such as Mars. Terrestrial impact structures excavated in basaltic targets provide the opportunity for analog studies. In Brazil, seven impact structures have been confirmed so far. Three of them, Vargeão Dome, Vista Alegre, and Cerro do Jarau, were formed in the same basaltic province belonging to the Paraná Basin, and they have several common characteristics. Oxidized basaltic breccias locally containing sandstone clasts occur in all these structures. In this work, selected samples of such breccias from the Vargeão Dome impact structure in southern Brazil were petrographically and geochemically investigated to further constrain the effects of the postimpact hydrothermal alteration. The breccia matrix shows typical oxidation effects induced by postimpact hydrothermal fluids, which highlight its heterogeneous nature, related to the impact event, and mixing components from different pre-impact stratigraphic formations. The detection of partially dissolved exsolution lamellae in pyroxene and of related alteration products constrains the effects of hydrothermal alteration in the basalts of the Vargeão Dome, which could serve as a terrestrial analog for planetary studies.
Shock effects in feldspars: An overview
ABSTRACT Feldspars are the dominant mineral in the crust of most terrestrial planetary bodies, including Earth, Earth’s moon, and Mars, as well as in asteroids, and thus in meteorites. These bodies have experienced large numbers of hypervelocity impact events, and so it is important to have a robust understanding of the effects of shock waves exerted on feldspars. However, due to their optical complexity and susceptibility to weathering, feldspars are underutilized as shock barometers and indicators of hypervelocity impact. Here, we provide an overview of the work done on shocked feldspars so far, in an effort to better frame the current strengths and weaknesses of different techniques, and to highlight some gaps in the literature.