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Contact metamorphism & fluids. Can fluid composition change during met?. Fluid composition. It can change composition during metamorphism Internally buffered Fluids evolved stay in system Top reaction, when do you leave the reaction line?. What if an open system?
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Fluid composition • It can change composition during metamorphism • Internally buffered • Fluids evolved stay in system • Top reaction, when do you leave the reaction line?
What if an open system? • Infiltrated by external fluids • What is fluid composition here?
Paths of buffered or open system fluidsalso note pressure changes
Calc-silicates • Marbles: pure carbonate • Calc-silicates: carbonate with silicates • Skarn: calc-silicate formed by metasomatism
Intrusion 1/2 Km
Talc Intrusion 1/2 Km
Intrusion Tremolite Talc 1/2 Km
Intrusion Forsterite Tremolite Talc 1/2 Km
Intrusion Periclase+Fo Forsterite Tremolite Talc 1/2 Km
+Pe +Fo +Tr Intrusion Periclase+Fo Forsterite Tremolite Talc 1/2 Km
Index minerals in calc-silicates • Talc • Tremolite • +/- diopside • Forsterite • Periclase • Monticellite
Ubehebe contact aureole • No talc zone, why?
Tremolite blossoms in silicious dolostone • Fluid along cracks, not pervasive
More evidence for localize fluid flow • Periclase zone
What sequence of index minerals if externally buffered fluid: • XCO2 = 0.5 • XCO2 = 0.05 • XCO2 = 0.9
What sequence of index minerals if low quartz content in protolith? • Which reactions? • Protolith: dolomite, calcite, some quartz • XCO2 < 0.6
Alta stock contact aureole ~31 Ma
Alta Contact Aureole at Albion Basin Index Minerals