Constraining conditions and mechanisms of the early stages exhumation from within subduction zones is challenging. Although pressure, temperature, age can be inferred exhumed rock record, it generally difficult to derive each these parameters any single rock, thus demanding assumptions that diverse data multiple samples safely combined into a pressure-temperature-time (P-T-t) path might then us...

An exotic block of garnet-bearing schist has been found at the boundary between Early Triassic Takinosawa Unit Nedamo Belt and Jurassic Nakatsugawa Complex North Kitakami Belt, NE Japan. This is only second discovery schists in Belt; previously identified occur early Carboniferous Tsunatori units Belt. The characterized by a mineral assemblage garnet + phengite epidote albite quartz titanite. P...

Abstract The Kawatuna area has a complex geological structure condition and is estimated to be weak zone for hydrothermal solutions rise then accumulate into deposits in the form of veins. Based on this, it makes this interesting study. This study aims determine its influence distribution veins area. method used surface mapping structures analysis. mapping, was found that composed schist rock u...

This study presents lithologic and petrogenetic investigation of bedded quartzite from Okemesi massive quartzites Ado-Ekiti in southwestern Nigeria. is extensive, thickly steeply dipping while hummocky, ferruginous, fractured, non-bedded. Analytical results reveal average SiO2 (94.74 %) (93.88%). Similarly, Rb/Sr are 0.74 1.22 Sr/Ba 0.89 0.69, respectively. These parameters portray them as supr...

The world-class Macraes orogenic gold deposit (∼10Moz resource) formed during the late metamorphic uplift of a metasedimentary schist belt in southern New Zealand. Mineralising fluids, metals and metalloids were derived from within the metasedimentary host. Helium and argon extracted from fluid inclusions in sulphide mineral grains (three crush extractions from one sample) have crustal signatur...

Soursat Metamorphic Complex (SMC) in west of Takab city is one of the polyphase metamorphic terrenes in northern Sanandaj-Sirjan metamorphic belt of Iran. The SMC composed mainly of metasedimentary rocks associated with granitic intrusions. Based on metamorphic rocks, two metamorphic phases could be separate in the complex. M1 is representative of regional metamorphisms which varies from greens...