FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023221508> ?p ?o ?g. }

• W2023221508 endingPage "240" @default.
• W2023221508 startingPage "233" @default.
• W2023221508 abstract "The relationship between structure and volcanism in the Tongariro Volcanic Centre, New Zealand, is largely masked by a mantle of young volcanic deposits. Here we report the results of an integrated geophysical investigation (using gravity, multi-level aeromagnetic and magnetotelluric methods) of subsurface deposits and structures in the upper 1–2 km across the axis of the Tongariro Volcanic Centre. Modelling of these data across the Tama Lakes saddle shows that the outcropping volcanic deposits are up to 800 m thick, underlain by Tertiary sediments (of a few 10's to a few 100 m in thickness) and in turn lying above a basement of probable Mesozoic greywacke. Basement faulting is shown to be concentrated in the centre of the rift, which is 18 km wide at this location, but no vertical offset is resolved at the rift axis. Vertical displacements on basement faults of 250–300 m are modelled giving a minimum total basement subsidence of 650 m. A 5 km-wide, deep low resistivity zone occurs at the axis of the rift which is interpreted as either resulting from extensive fracturing and/or hydrothermal alteration within the basement. Steep-sided volcanic bodies with a high proportion of lavas/dykes coincide with the Waihi fault and the rift axis. Coincidence with the Waihi Fault suggests that this fault system may have provided magma pathways to the surface and a focus for dyke emplacement, which could have contributed to rift extension. The lack of offset at the rift axis may reflect the juvenile nature of faulting at this location, which is consistent with the notion of a migration of faulting towards the centre of the graben, alternatively, rifting may have been entirely accommodated by dyke emplacement." @default.
• W2023221508 created "2016-06-24" @default.
• W2023221508 creator A5019260242 @default.
• W2023221508 creator A5030783820 @default.
• W2023221508 creator A5042246686 @default.
• W2023221508 creator A5061955264 @default.
• W2023221508 date "2009-01-01" @default.
• W2023221508 modified "2023-09-26" @default.
• W2023221508 title "Subsurface structure across the axis of the Tongariro Volcanic Centre, New Zealand" @default.
• W2023221508 cites W1500787922 @default.
• W2023221508 cites W1604609679 @default.
• W2023221508 cites W1675451487 @default.
• W2023221508 cites W1974399179 @default.
• W2023221508 cites W1985538365 @default.
• W2023221508 cites W1995083048 @default.
• W2023221508 cites W2001680486 @default.
• W2023221508 cites W2003076733 @default.
• W2023221508 cites W2008271438 @default.
• W2023221508 cites W2010649331 @default.
• W2023221508 cites W2010943359 @default.
• W2023221508 cites W2014970528 @default.
• W2023221508 cites W2021256246 @default.
• W2023221508 cites W2044812716 @default.
• W2023221508 cites W2050775631 @default.
• W2023221508 cites W2054544937 @default.
• W2023221508 cites W2058881675 @default.
• W2023221508 cites W2059342515 @default.
• W2023221508 cites W2059712778 @default.
• W2023221508 cites W2059722957 @default.
• W2023221508 cites W2063004740 @default.
• W2023221508 cites W2066294087 @default.
• W2023221508 cites W2066621896 @default.
• W2023221508 cites W2068015389 @default.
• W2023221508 cites W2068646218 @default.
• W2023221508 cites W2075541277 @default.
• W2023221508 cites W2078816475 @default.
• W2023221508 cites W2078838424 @default.
• W2023221508 cites W2094773406 @default.
• W2023221508 cites W2108982325 @default.
• W2023221508 cites W2110142704 @default.
• W2023221508 cites W2115498780 @default.
• W2023221508 cites W2117948842 @default.
• W2023221508 cites W2118153886 @default.
• W2023221508 cites W2129221669 @default.
• W2023221508 cites W2149397190 @default.
• W2023221508 cites W2159367216 @default.
• W2023221508 doi "https://doi.org/10.1016/j.jvolgeores.2008.11.017" @default.
• W2023221508 hasPublicationYear "2009" @default.
• W2023221508 type Work @default.
• W2023221508 sameAs 2023221508 @default.
• W2023221508 citedByCount "22" @default.
• W2023221508 countsByYear W20232215082012 @default.
• W2023221508 countsByYear W20232215082016 @default.
• W2023221508 countsByYear W20232215082017 @default.
• W2023221508 countsByYear W20232215082018 @default.
• W2023221508 countsByYear W20232215082020 @default.
• W2023221508 countsByYear W20232215082021 @default.
• W2023221508 countsByYear W20232215082022 @default.
• W2023221508 countsByYear W20232215082023 @default.
• W2023221508 crossrefType "journal-article" @default.
• W2023221508 hasAuthorship W2023221508A5019260242 @default.
• W2023221508 hasAuthorship W2023221508A5030783820 @default.
• W2023221508 hasAuthorship W2023221508A5042246686 @default.
• W2023221508 hasAuthorship W2023221508A5061955264 @default.
• W2023221508 hasConcept C120806208 @default.
• W2023221508 hasConcept C127313418 @default.
• W2023221508 hasConcept C127413603 @default.
• W2023221508 hasConcept C147176958 @default.
• W2023221508 hasConcept C165205528 @default.
• W2023221508 hasConcept C169212394 @default.
• W2023221508 hasConcept C17409809 @default.
• W2023221508 hasConcept C175551986 @default.
• W2023221508 hasConcept C192241223 @default.
• W2023221508 hasConcept C2776761171 @default.
• W2023221508 hasConcept C2781297371 @default.
• W2023221508 hasConcept C32848823 @default.
• W2023221508 hasConcept C49708893 @default.
• W2023221508 hasConcept C50682988 @default.
• W2023221508 hasConcept C5900021 @default.
• W2023221508 hasConcept C6363049 @default.
• W2023221508 hasConcept C77928131 @default.
• W2023221508 hasConceptScore W2023221508C120806208 @default.
• W2023221508 hasConceptScore W2023221508C127313418 @default.
• W2023221508 hasConceptScore W2023221508C127413603 @default.
• W2023221508 hasConceptScore W2023221508C147176958 @default.
• W2023221508 hasConceptScore W2023221508C165205528 @default.
• W2023221508 hasConceptScore W2023221508C169212394 @default.
• W2023221508 hasConceptScore W2023221508C17409809 @default.
• W2023221508 hasConceptScore W2023221508C175551986 @default.
• W2023221508 hasConceptScore W2023221508C192241223 @default.
• W2023221508 hasConceptScore W2023221508C2776761171 @default.
• W2023221508 hasConceptScore W2023221508C2781297371 @default.
• W2023221508 hasConceptScore W2023221508C32848823 @default.
• W2023221508 hasConceptScore W2023221508C49708893 @default.
• W2023221508 hasConceptScore W2023221508C50682988 @default.
• W2023221508 hasConceptScore W2023221508C5900021 @default.
• W2023221508 hasConceptScore W2023221508C6363049 @default.
• W2023221508 hasConceptScore W2023221508C77928131 @default.

• next