Colin Bryden
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M.Sc. Thesis
(PDF - 34 Mb)
Scapolite ((Ca, Na)4Al3-6Si6-9O24(SO4, CO3, Cl)), a volatile-bearing framework silicate, is found in pegmatites and leucosomes in close field association with (ultra)-high pressure ((U)HP) eclogites in the Nord酶yane domain of the Western Gneiss Region (WGR) of Norway. Study of the field relationships, stable isotope geochemistry, and geochronology of these scapolite-bearing rocks provides insights into the role of fluids in partial melting of (U)HP rocks during the Scandian Orogeny (425-380 Ma). Scapolitebearing pegmatites in Nord酶yane were divided into three types based on mineralogy, texture, and scapolite chemistry. The most abundant Type 1 pegmatites are associated with granodioritic rocks which cut amphibolite-facies fabrics in adjacent basement gneisses and host numerous eclogite bodies. The pegmatites, which are concentrated in low-strain areas, are interpreted as a late-stage differentiate of the granodiorites. Scapolites from Type 1, 2 and 3 pegmatites, and basement leucosomes, all share similar 未13C (-7.97 to -2.24 鈥�) and 未34S (-1.1 to 5.7鈥�) compositions, interpreted to indicate a common source of volatiles, derived from the mantle. Type 1 pegmatites crystallized at ~ 395 Ma under amphibolite-facies conditions (ca. 750 掳C, assuming P = 1.0 GPa), at the same time as Type 3 pegmatites (396卤2 Ma; Gordon et al., 2013). An older ~ 420 Ma subpopulation of titanites is interpreted as inherited, likely from adjacent basement gneisses. Scapolite 未18O (16.21 to 20.05鈥�) and titanite 蔚Nd (-6.8 to -10.8) values indicate that Type 1 pegmatites crystallized from a crustal melt, suggesting that the introduction of mantle fluids promoted melting of crustal rocks. Mantle fluids are interpreted to have infiltrated subducted Baltican continental crust during subduction (ca.415-400 Ma), or in the early stages of extension and exhumation (ca. 399-395 Ma). These fluids may have been present in Laurentian lithospheric mantle prior to the Caledonian orogeny, or introduced from the down-going slab during early Caledonian subduction.
Keywords: (Ultra)-High Pressure, Partial Melting, Scapolite
Pages: 303
Supervisor: Rebecca Jamieson