FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2020366947> ?p ?o ?g. }

• W2020366947 endingPage "43" @default.
• W2020366947 startingPage "21" @default.
• W2020366947 abstract "The Early Devonian Boggy Plain Supersuite is a belt of I‐type granitic and volcanic rocks extending for over 500 km in the central Lachlan Fold Belt. It has a distinctive composition and origin. Compared with other Lachlan Fold Belt I‐types, rocks of the supersuite are high in Cu and incompatible elements (K, Ba, Sr, Rb, La, Ce, U, and Th). The source for the magmas is interpreted to have been an incompatible element‐rich gabbroic layer, underplated at the base of the crust in the Ordovician. This layer is inferred to correspond to a belt of Ordovician shoshonitic basaltic volcanic rocks that has a strikingly similar geographical distribution to the supersuite. Compositional variation in the supersuite is ascribed to fractional crystallization, in contrast to most other I‐type magmas of the Lachlan Fold Belt which owe most of their compositional variation to fractionation by restite unmixing. This contrast resulted from differences in source rocks, with the Boggy Plain Supersuite being derived from basaltic sources at high temperatures, and the restite‐bearing I‐types being derived from more felsic sources at lower temperatures. The proposed crustal source for the supersuite magmas is consistent with the orogenic evolution in the Lachlan Fold Belt being mainly related to reworking of pre‐existing crust, and has no analogy in the evolution of modern continental margin orogenic zones. Fractional crystallization of Boggy Plain Supersuite magmas produced rock types ranging from pyroxene‐rich and plagioclase‐rich gabbroic cumulates, through pyroxene‐bearing quartz monzodiorites and granodiorites to high‐silica granites. The latter represent the fractionated liquid removed during the crystallization of the more mafic cumulates. These liquids vary due to additional fractionation. The supersuite is particularly prospective for Cu and Au mineralization associated with the more mafic intrusives, and W and Bi in the most fractionated felsic bodies." @default.
• W2020366947 created "2016-06-24" @default.
• W2020366947 creator A5004584223 @default.
• W2020366947 creator A5004747551 @default.
• W2020366947 creator A5062931133 @default.
• W2020366947 date "1987-03-01" @default.
• W2020366947 modified "2023-10-01" @default.
• W2020366947 title "The Boggy Plain Supersuite: A distinctive belt of I‐type igneous rocks of potential economic significance in the Lachlan Fold Belt" @default.
• W2020366947 cites W1970922317 @default.
• W2020366947 cites W1985240321 @default.
• W2020366947 cites W1985739136 @default.
• W2020366947 cites W1990533710 @default.
• W2020366947 cites W1998191793 @default.
• W2020366947 cites W2002909355 @default.
• W2020366947 cites W2012283725 @default.
• W2020366947 cites W2018990680 @default.
• W2020366947 cites W2026475967 @default.
• W2020366947 cites W2031650492 @default.
• W2020366947 cites W2036612379 @default.
• W2020366947 cites W2037838634 @default.
• W2020366947 cites W2039323682 @default.
• W2020366947 cites W2040360057 @default.
• W2020366947 cites W2042803182 @default.
• W2020366947 cites W2063205632 @default.
• W2020366947 cites W2069148099 @default.
• W2020366947 cites W2079569144 @default.
• W2020366947 cites W2080900129 @default.
• W2020366947 cites W2094414596 @default.
• W2020366947 cites W2105250272 @default.
• W2020366947 cites W2112195993 @default.
• W2020366947 cites W2114174305 @default.
• W2020366947 cites W2132888677 @default.
• W2020366947 cites W2148187106 @default.
• W2020366947 cites W2152410369 @default.
• W2020366947 cites W2164054892 @default.
• W2020366947 cites W2314338517 @default.
• W2020366947 cites W2338158576 @default.
• W2020366947 cites W4205749704 @default.
• W2020366947 doi "https://doi.org/10.1080/08120098708729392" @default.
• W2020366947 hasPublicationYear "1987" @default.
• W2020366947 type Work @default.
• W2020366947 sameAs 2020366947 @default.
• W2020366947 citedByCount "83" @default.
• W2020366947 countsByYear W20203669472012 @default.
• W2020366947 countsByYear W20203669472013 @default.
• W2020366947 countsByYear W20203669472015 @default.
• W2020366947 countsByYear W20203669472016 @default.
• W2020366947 countsByYear W20203669472017 @default.
• W2020366947 countsByYear W20203669472018 @default.
• W2020366947 countsByYear W20203669472019 @default.
• W2020366947 countsByYear W20203669472020 @default.
• W2020366947 countsByYear W20203669472021 @default.
• W2020366947 countsByYear W20203669472022 @default.
• W2020366947 countsByYear W20203669472023 @default.
• W2020366947 crossrefType "journal-article" @default.
• W2020366947 hasAuthorship W2020366947A5004584223 @default.
• W2020366947 hasAuthorship W2020366947A5004747551 @default.
• W2020366947 hasAuthorship W2020366947A5062931133 @default.
• W2020366947 hasConcept C11872896 @default.
• W2020366947 hasConcept C120806208 @default.
• W2020366947 hasConcept C127313418 @default.
• W2020366947 hasConcept C127413603 @default.
• W2020366947 hasConcept C151730666 @default.
• W2020366947 hasConcept C161509811 @default.
• W2020366947 hasConcept C167284885 @default.
• W2020366947 hasConcept C17409809 @default.
• W2020366947 hasConcept C192241223 @default.
• W2020366947 hasConcept C193429443 @default.
• W2020366947 hasConcept C2776698055 @default.
• W2020366947 hasConcept C2778998827 @default.
• W2020366947 hasConcept C2779181077 @default.
• W2020366947 hasConcept C2779870107 @default.
• W2020366947 hasConcept C2780364934 @default.
• W2020366947 hasConcept C42787717 @default.
• W2020366947 hasConcept C53942344 @default.
• W2020366947 hasConcept C5900021 @default.
• W2020366947 hasConcept C78519656 @default.
• W2020366947 hasConceptScore W2020366947C11872896 @default.
• W2020366947 hasConceptScore W2020366947C120806208 @default.
• W2020366947 hasConceptScore W2020366947C127313418 @default.
• W2020366947 hasConceptScore W2020366947C127413603 @default.
• W2020366947 hasConceptScore W2020366947C151730666 @default.
• W2020366947 hasConceptScore W2020366947C161509811 @default.
• W2020366947 hasConceptScore W2020366947C167284885 @default.
• W2020366947 hasConceptScore W2020366947C17409809 @default.
• W2020366947 hasConceptScore W2020366947C192241223 @default.
• W2020366947 hasConceptScore W2020366947C193429443 @default.
• W2020366947 hasConceptScore W2020366947C2776698055 @default.
• W2020366947 hasConceptScore W2020366947C2778998827 @default.
• W2020366947 hasConceptScore W2020366947C2779181077 @default.
• W2020366947 hasConceptScore W2020366947C2779870107 @default.
• W2020366947 hasConceptScore W2020366947C2780364934 @default.
• W2020366947 hasConceptScore W2020366947C42787717 @default.
• W2020366947 hasConceptScore W2020366947C53942344 @default.
• W2020366947 hasConceptScore W2020366947C5900021 @default.
• W2020366947 hasConceptScore W2020366947C78519656 @default.
• W2020366947 hasIssue "1" @default.
• W2020366947 hasLocation W20203669471 @default.

• next