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- W1609908923 abstract "Iron meteorites may seem to present a challenge for I-Xe dating because it is the inclusions, not the metal, that contains the iodine; therefore, it is the inclusions that are dated, not the metal. However, this is a good thing since different minerals close at different times, providing diverse ages and the potential for cooling rate information. Silicate inclusions are frequent only in types IAB and IIE, and earlier studies demonstrate that diverse I-Xe systems can survive intact in these inclusions, preserving a spectrum of age information [1–5]. An early study of noble gases from Campo del Cielo IA (El Taco mass) was done on separated silicate inclusions which were crushed, sieved and chemically treated, but not irradiated. That work [6] confirmed that silicate inclusions indeed contain excess Xe, but specific carrier phases were not identified. Our previous studies [7] involved a silicategraphite-metal inclusion (SiGrMet) from Campo del Cielo in a slice from the Museum of Natural History, Vienna, which demonstrated presence of radiogenic 129 Xe in two different silicates [7]. Eight different 300×300μm laser-raster excavations were made, each approximately 12 μm deep. Typical raster areas are shown in Fig. 1 (data in Table 1). As expected, no radiogenic Xe was found in the metal itself, nor was it found in the rust or in the olivine. These particular silicates contained Xe that was nearly monoisotopic Xe, with almost no measurable trapped Xe." @default.
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- W1609908923 date "2009-03-01" @default.
- W1609908923 modified "2023-09-24" @default.
- W1609908923 title "I-Xe System in Campo del Cielo Silicates" @default.
- W1609908923 hasPublicationYear "2009" @default.
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