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Fluid inclusions in mantle xenoliths
Lithos, 2001Abstract Fluid inclusions in olivine and pyroxene in mantle-derived ultramafic xenoliths in volcanic rocks contain abundant CO2-rich fluid inclusions, as well as inclusions of silicate glass, solidified metal sulphide melt and carbonates. Such inclusions represent accidentally trapped samples of fluid- and melt phases present in the upper mantle, and
Tom Andersen, Else-Ragnhild Neumann
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Noble gases in an Hawaiian xenolith
Nature, 1975THE noble gas record in meteorites and lunar samples has been the subject of many investigations aimed at determining their age, the history of their exposure to cosmic rays and to the solar wind, and the early chronology of events in the Solar System (see review in ref. 1).
E. W. HENNECKE, O. K. MANUEL
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Science China. Earth Sciences, 2020
Jianping Zheng, B. Xia, H. Dai, Qiang Ma
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Jianping Zheng, B. Xia, H. Dai, Qiang Ma
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XENOLITHS AT THRELKELD, CUMBERLAND
Proceedings of the Yorkshire Geological Society, 1940In the years 1925–6 I did a good deal of field-work on the so-called microgranite of Threlkeld and St. John’s Vale, with the intention of making a complete petrographic investigation of these rock masses. Material was collected and a number of microscope slices were cut.
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Southern African Kimberlites and their Xenoliths
1991South African diamonds were found in primary kimberlite source rock in the late 1860’s and early 1870’s when Jagersfontein, Bultfontein, DeBeers, Dutoitspan, and other pipes near Kimberley (Fig. 1) were discovered in rapid succession (Wilson 1982; Janse 1984). Prior to this, stream gravels were the only diamond source worldwide.
J. J. Gurney +5 more
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Farmington Meteorite: Cristobalite Xenoliths and Blackening
Science, 1967The Farmington chondrite contains two small xenoliths of granular cristobalite, each surrounded by a thin reaction rim of diopsidic clinopyroxene. Similarities between the blackened structure and drusy cavities, characteristic of this meteorite, and those of an experimentally heat-treated chondrite suggest that Farmington was reheated rather than ...
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A Xenolithic Pegmatite in the Dalbeattie “Granite”
Geological Magazine, 1936SUMMARY AND CONCLUSIONA pegmatite cutting granodiorite contains abundant xenoliths which are in various stages of assimilation. Assimilation involved the conversion by the process of “reciprocal reaction” of the minerals of the xenoliths into species which were in equilibrium under the prevailing magmatic conditions, and the subsequent “mechanical ...
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