By Bernhard J. Knipping, Ralph B. Phillips
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However, it is composed predominantly of goethite, in part with hematite, and submicroscopic clay minerals (TROVER 1967). , dikes
K) = 3000 R Fig. 5 The most extreme points of those shown in fig. 3 for one rock type were connected in order to clarify the range of variation in the chemical composition of the different basalts from the Werra mining district (further explanation in text). 59 The resets of the microscopy are largely confirmed when the results of the chemical analyses are depicted in this way. The following statements can be made based on this evaluation: 1. , titanaugite, plagioclase). 2. Similarities in the conditions of formation are underscored by the overlapping areas in the R1-R2 diagram covered by the studied olivine nephefinites, limburgites, and basanites (fig.
Yet, they may reach sizes of over 1 cm in the hornblende-bearing basanite of dike