The UCS and UTS values for clinopyroxenite and serpentinite falls in category of strong rocks while hornblendite and garnet granulite
sample shows relatively weak character.
The Sigula fault-related dyke-like gabbro-diabase is located in the Tallinn domain and the ellipse-shaped Abja quartz monzodiorite lies within the southern Estonian granulite
Knudsen, "Petrology and geothermobarometry of granulite
facies metapelites from the Hisoy-Torungen area, south Norway: New data on the Sveconorvegian P-T-t path of the Bamble sector," Journal of Metamorphic Geology, vol.
The 1,742 Ma age we obtained for the zircon inclusion in the greenish blue sapphire coincides with the age of zircons possibly derived from granulites
found, for example, in southern Madagascar (Kroner et al., 1999).
One might suppose that the middle crust in the SG-3 area can be represented by rocks similar in age and composition of the protoliths to the SG-3 Archaean complex but metamorphosed under conditions of high-temperature amphibolite and granulite
950, bronze), Metropolitan Museum of Art in New York ( Umamaheshvara, 11th century, copper alloy), Cleveland Museum of Art in Ohio (Shiva as Brahma, 10-11th century, granite), Dallas Museum of Art in Texas (Shiva Nataraja, 11th century, bronze), Museum of Fine Arts Boston in Massachusetts (Shiva, late 10th century, granulite
), Los Angeles County Museum of Art in California (Shiva's Family, 10th century), Philadelphia Museum of Art in Pennsylvania (Shiva as Bhairava, 11-12th century, granitic stone), Art Institute of Chicago in Illinois (Dakshinamurti, 10th century, granite), Nelson-Atkins Museum of Art Kansas City in Missouri (Shiva Nataraja, 13th century), etc .
According to APEC a detailed exploration programme is being initiated on the property, located to the southeast of Canaco Resources Inc's major gold discovery, which was recognised last summer as a new geological setting (high grade granulite
facies metamorphic terrain) that can produce sizable mineralised deposits.
 Chetty .T.R.K .1996, " Proterozoic zones in southern granulite
terrain" Gondwana Research group memoir 3 , 77-89
This structure consists of a Proterozoic-age vanadiumrich sedimentary series metamorphosed to the granulite
facies but most commonly found as retrograde kyanite-almandine-subfacies rocks of the upper amphibolite facies.
In support of this model, Collins (2002) points out that the mineralogy of many granulite
facies complexes requires geothermal gradients between 20[degrees] and 50[degrees]C per km, which is much higher than gradients in collisional environments, but is consistent with those expected in backarc settings.