What Is Older Granite That Intruded Or Gneiss

The rock in the lower hill in the foreground is gneiss and migmatite of the the highly metamorposed and intruded skagit gneiss complex part of the chelan mountains terrane.

What is older granite that intruded or gneiss.

A gently sloping contact between the granite and the older overlying gneiss and schist can be seen in cliffs along canyons east of the continental divide where also light colored pegmatite veins extend in all directions through the gneiss and schist. Massive fine grained phases discordantly intrude massive coarse grained phases which are concordant with the older augen gneiss. Mt crawford granite gneiss hypothesis 4 the granitic gneiss is an early delamerian granite intruded during or just before the first phase of delamerian deformation similar to the rathjen gneiss. All these rock types can be observed at close hand along trails in these areas.

Interpreted as having been intruded into original grenville series. The presence of two generations of granitic rocks in the gneiss domes he examined led eskola to suggest that the gen eral condition for gneiss dome formation is the superposition of two orogenic events. 8 10 37 table pl. Was probably an intrusive magma with gradational contacts or a mobilized component of the metasomatic microcline augen gneiss.

Similar to alaskite gneiss but with more than 3 dark minerals. Gneiss dome core consists of older prekinematic granites and coeval synkinematic migmatite intruded during gneiss dome formation. Has pronounced phacoidal texture. Granite intruded into mafic dikes which in turn cross cut granite.

Irregular bodies of granite gneiss are interleaved with the layered gneisses in the northern part of the teton range. Which is older and why. Sterling igneous suite granite gneiss pale pink to gray medium grained granite gneiss commonly with small porphyroclasts of microcline orthoclase. The granite gneiss is relatively coarse grained streaky gray or pink and composed principally of quartz feldspar biotite and hornblende.

The golden horn granite is different from the older plutonic rocks of the north cascades crystalline core the golden horn rock is a true granite with a high amount. The gneiss is older because it had to exist before it was intruded by the granite. You go to mount rushmore and see a blob of what appears to be black granite in that beautiful white gneiss. It differs from enclosing layered gneisses in its coarser texture lack of layering.

Miller described hawkeye granite as a facies of his lyon mountain granite but it is here considered to be an older spearate unit.