By Bernhard J. Knipping, Ralph B. Phillips
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Extra resources for Basalt intrusions in evaporites
The studied rocks generally have a porphyritic texture. Deviations from this are also noted. Olivine Xenomorphic olivine occurs as aggregates in several basaltic rocks (dikes
Il( O.! e e l = t - / alkali-s" % O0 . '" . L"/" , fephnte •. ~lt ,~ • ~ phonolite n . s •" "'-. o # phonolite , / s" ..... / trachyte t / I 7' / ......... -1000 t ' ~ trachy- • ,s s J ........... " basalt. ¢ . ~ • ; Lati- I ; f - " ~s~ hawaiite# , andesi-basalt v ~ i basalt mugearite "" - ~-r'" / tholeiite t Il # I .... -"" _ . :'~"" dacite • .... ,,""" rhyodacite quartz* trachyte 10'00 t . - , ~des,e', ~ '#-. . . . ~ s / # • "~-. "- - "" rhyolite ...... ~------. alkali - rhyolite t. . . .
Samples from dike and sample 46/86 (dike
) were not able to be classified due to intense autometamorphism (nc = not classified). , homblende basanite, nepheline, basanite, basanitic alkali-olivine basalt) was not attempted because of the gradual transitions between the individual basalt types found in the working area. The rock of dike
Basalt intrusions in evaporites by Bernhard J. Knipping, Ralph B. Phillips