References35.96 · Montanuniversit?t Leoben+ 448.63 · Goethe-Universit?t Frankfurt am Main32.61 · Bundesanstalt für Geowissenschaften und RohstoffeShow
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CitationsCitations0ReferencesReferences58ABSTRACT: Palaeoproterozoic sequences deformed during the 1600Ma Olary and Isa orogenies in the Broken Hill and Mount Isa terranes preserve an earlier record of syn-extensional magmatism, deformation and low-pressure/high-temperature metamorphism linked to basin formation and normal faulting at upper crustal levels. Crustal extension occurred nearly continuously from 1800 to 1640Ma and produced several stacked sedimentary basins, the content of which was mainly controlled by growth faulting along the margins of NNW- and NW-trending half-graben. Mid-crustal magmatic rocks intruded and unroofed during the course of extension are commonly mylonitised and were carried to higher structural levels on extensional shear zones active at the time of sedimentation. Metamorphic monazite ages from deformed host rocks of the syn-extensional Sybella Granite at Mount Isa support this interpretation and include a 1675Ma population that is much too old to be related to either later crustal shortening or the Isan orogeny. This record of near continuous extension at upper and mid-crustal levels is difficult to reconcile with existing reconstructions of Rodinia in which the Broken Hill and Mount Isa terranes are juxtaposed against rocks of similar age in southwest Laurentia that preserve a history of contractional deformation related to terrane accretion, amalgamation and collision. Equally difficult to reconcile are palaeogeographical reconstructions of Australia which place the Broken Hill and Mount Isa terranes adjacent to each other in a back-arc position while maintaining an along-strike continuity with the rocks of southwest Laurentia. In such a configuration, the Mojave, Yavapai, and Mazatzal provinces lie south of the proposed common Palaeoproterozoic suture (Cheyenne Belt) whereas their inferred age equivalents in the Broken Hill and Mount Isa terranes lie north of this former convergent plate margin. An alternative reconstruction of Proterozoic eastern Australia is proposed in which back-arc extension in the Broken Hill and Mount Isa terranes was linked to retreat of a west-dipping (present-day coordinates) subduction zone and associated magmatic arc that now resides partially or wholly within North America. Eastern Australia and Laurentia ceased to be part of a single continental landmass soon after 1800Ma and thereafter followed increasingly divergent tectonic paths until re-amalgamated during collision at ca. 1600Ma. Extension in the Broken Hill and Mount Isa terranes produced a North American Basin-and-Range-style crustal architecture that has no obvious counterpart in southwest Laurentia.Article · Oct 2008 +1 more author ...ABSTRACT: The redox boundary for temperatures up to 600°C and pressures up to 4000 bar has been calculated using the “revised HKF model” for the prediction of the molal Gibbs free energy of formation at elevated pressures and temperatures. The results indicate that the oxygen fugacity (fO2) at which trivalent Eu is reduced to Eu2+ increases with increasing temperature. Thus, in high-temperature regimes Eu can be fractionated from the other REE.If in fluid-rock interaction under mildly acidic conditions the REE pattern of the fluid is controlled by sorption processes, the decreasing ionic radius from La to Lu leads to , and, provided Eu occurs as Eu2+, to a positive Eu anomaly (compared to the source-rock for the REE) in the fluid. Under nearly neutral to mildly basic conditions the REE pattern of the same fluid is governed by complexation mechanisms with carbonate, fluoride and hydroxide complexes being the most important REE species. This leads to . Because complexation extends the stability of Eu3+ towards lower fO2, reduction to Eu2+ under mildly basic conditions is limited to more reducing environments.Since the REE content of alteration fluids is extremely low, alteration of whole-rock REE patterns during hydrothermal or metamorphic fluid-rock interaction is rather ineffective, unless the water/rock ratio is ? 102–103 or infiltration metasomatism is severe. Apart from these situations, REE systematics should not be affected by hydrothermal or metamorphic fluid-rock interaction.Article · Dec 1991 ABSTRACT: This paper presents a table of abundances of the elements in the various major units of the Earth's lithic crust with a documentation of the sources and a discussion of the choice of units and data.Article · Jan 1961
Full-text · Article · Dec 2014 +4 more authors ... Full-text · Article · Nov 2005 +2 more authors ... Full-text · Article · Apr 2002 Data provided are for informational purposes only. Although carefully collected, accuracy cannot be guaranteed. Publisher conditions are provided by RoMEO. Differing provisions from the publisher's actual policy or licence agreement may be applicable.This publication is from a journal that may support self archiving.Last Updated: 19 Oct 16
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