FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4293661471> ?p ?o ?g. }

• W4293661471 abstract "&lt;p&gt;The India-Asia collision can have only a limited role as an actualistic model for the closure of Western Tethys and the subsequent Alpine orogenies because the impacting margins appear to have been sub-parallel and rather regular and the intervening ocean seems to have contained few volcanic edifices or continental fragments. A better guide to possible pre-collision processes is provided by the incipient Australia &amp;#8211; Southeast Asia collision, which has already proved its worth as a key area for the study of small extensional zones within overall compressional environments. Insights into the possible roles of ridge-related features during oceanic closure are now being obtained from studies in the northern part of the Philippines Archipelago, which was largely formed by post-Middle Cretaceous volcanic activity associated with subduction of oceanic crust from both east and west. Double-sided subduction inevitably produces geomorphological complexity, but not all the anomalous features of the Philippines can be attributed to this cause. A sharp bend in topographic trends involving most of the southern part of the island of Luzon is here interpreted as a consequence of the impact on the east-facing subduction zone of the Anagolay volcanic massif formed by hot-spot volcanism associated with the spreading ridge in the West Philippine Basin. This bend can be considered a small-scale analogue of the syntaxes that define the limits of the India-Asia collision and demonstrates the way in which the presence of even a relatively small region of thickened crust can influence the morphology of an entire collision zone. Similar processes must have operated in other Alpino-type orogenic belts but may be hard to recognise because the generative units are no longer observable and their effects may be partly concealed by later tectonic over-printing.&lt;/p&gt;" @default.
• W4293661471 created "2022-08-31" @default.
• W4293661471 creator A5048321492 @default.
• W4293661471 creator A5091266626 @default.
• W4293661471 date "2022-08-30" @default.
• W4293661471 modified "2023-09-24" @default.
• W4293661471 title "Anagolay: the shape of the Philippines and the Luzon Syntaxis" @default.
• W4293661471 doi "https://doi.org/10.5194/egusphere-alpshop2022-56" @default.
• W4293661471 hasPublicationYear "2022" @default.
• W4293661471 type Work @default.
• W4293661471 citedByCount "0" @default.
• W4293661471 crossrefType "posted-content" @default.
• W4293661471 hasAuthorship W4293661471A5048321492 @default.
• W4293661471 hasAuthorship W4293661471A5091266626 @default.
• W4293661471 hasConcept C111368507 @default.
• W4293661471 hasConcept C120806208 @default.
• W4293661471 hasConcept C121704057 @default.
• W4293661471 hasConcept C127313418 @default.
• W4293661471 hasConcept C136137745 @default.
• W4293661471 hasConcept C151730666 @default.
• W4293661471 hasConcept C154200439 @default.
• W4293661471 hasConcept C160776313 @default.
• W4293661471 hasConcept C165205528 @default.
• W4293661471 hasConcept C1965285 @default.
• W4293661471 hasConcept C204207459 @default.
• W4293661471 hasConcept C2776698055 @default.
• W4293661471 hasConcept C32277403 @default.
• W4293661471 hasConcept C38652104 @default.
• W4293661471 hasConcept C41008148 @default.
• W4293661471 hasConcept C58097730 @default.
• W4293661471 hasConcept C63379926 @default.
• W4293661471 hasConcept C6363049 @default.
• W4293661471 hasConcept C75643213 @default.
• W4293661471 hasConcept C77928131 @default.
• W4293661471 hasConceptScore W4293661471C111368507 @default.
• W4293661471 hasConceptScore W4293661471C120806208 @default.
• W4293661471 hasConceptScore W4293661471C121704057 @default.
• W4293661471 hasConceptScore W4293661471C127313418 @default.
• W4293661471 hasConceptScore W4293661471C136137745 @default.
• W4293661471 hasConceptScore W4293661471C151730666 @default.
• W4293661471 hasConceptScore W4293661471C154200439 @default.
• W4293661471 hasConceptScore W4293661471C160776313 @default.
• W4293661471 hasConceptScore W4293661471C165205528 @default.
• W4293661471 hasConceptScore W4293661471C1965285 @default.
• W4293661471 hasConceptScore W4293661471C204207459 @default.
• W4293661471 hasConceptScore W4293661471C2776698055 @default.
• W4293661471 hasConceptScore W4293661471C32277403 @default.
• W4293661471 hasConceptScore W4293661471C38652104 @default.
• W4293661471 hasConceptScore W4293661471C41008148 @default.
• W4293661471 hasConceptScore W4293661471C58097730 @default.
• W4293661471 hasConceptScore W4293661471C63379926 @default.
• W4293661471 hasConceptScore W4293661471C6363049 @default.
• W4293661471 hasConceptScore W4293661471C75643213 @default.
• W4293661471 hasConceptScore W4293661471C77928131 @default.
• W4293661471 hasLocation W42936614711 @default.
• W4293661471 hasOpenAccess W4293661471 @default.
• W4293661471 hasPrimaryLocation W42936614711 @default.
• W4293661471 hasRelatedWork W1967565130 @default.
• W4293661471 hasRelatedWork W1981700868 @default.
• W4293661471 hasRelatedWork W2002670723 @default.
• W4293661471 hasRelatedWork W2022784417 @default.
• W4293661471 hasRelatedWork W2471286521 @default.
• W4293661471 hasRelatedWork W2983224063 @default.
• W4293661471 hasRelatedWork W3087164276 @default.
• W4293661471 hasRelatedWork W393953572 @default.
• W4293661471 hasRelatedWork W4293661471 @default.
• W4293661471 hasRelatedWork W2506500755 @default.
• W4293661471 isParatext "false" @default.
• W4293661471 isRetracted "false" @default.
• W4293661471 workType "article" @default.