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Geological model of the Lower Silesia ophiolite, proposed on the basis of geochemical and mineralogical study of mafic rocks, including rodingites* produced from boninite-type protolith and metarodingites formed at the expense of a plagiogranite. |
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Geological model of the Lower Silesia ophiolite, proposed on the basis of geochemical and mineralogical study of mafic rocks, including rodingites* produced from boninite-type protolith and metarodingites formed at the expense of a plagiogranite. |
* rodingite - metasomatic rock, a “by-product”of the ultramafic rock serpentinisation.
