FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2080862693> ?p ?o ?g. }

• W2080862693 endingPage "39" @default.
• W2080862693 startingPage "21" @default.
• W2080862693 abstract "Abstract A 65 km seismic reflection transect was shot in 1998 across Mackenzie Basin to Mount Cook Village, South Island, New Zealand, to provide a detailed image of the crustal structure in the central Southern Alps. The first 5 s (two‐way time (TWT)) of data were processed separately, with a maximum offset of 14 km for each shot, to image the upper 12–15 km of the crust. Data were processed as one continuous section, although the line was physically segmented due to an area of relatively steep topography with no vehicular access. No major, continuous regional‐scale features > 10 km are present in the data, but numerous 2–3 km scale reflections and discontinuities occur which are consistent with the known geology of monotonous greywacke sequences overlying schist. Strong, well‐defined reflections mark the active Irishman Creek Fault and confirm it to be a southeasterly dipping reverse fault with c. 1300–1700 m of Late Cretaceous‐Pleistocene sediments preserved in the footwall and an uplifted greywacke basement “high” in the hanging wall. Some evidence exists for active faults beneath latest Quaternary gravels at the Jollie valley and Tekapo River. Oppositely dipping reflections and discontinuities define a large, c. 15 km wavelength antiform beneath Tasman valley and Mount Cook that is imaged to 10 ± 2 km depths (3.5 s TWT). Two “end‐member” interpretations are consistent with the seismic data observations, velocity models, and constraining features of exposed geology, and extend existing geological cross‐sections to 10–15 km depth. One interpretation assumes imaged structures are primarily backthrusts developed in response to distributed Cenozoic deformation southeast of the Alpine Fault plate boundary, incorporating features observed in contemporary geodetic strain and numerical plate boundary models. The second interpretation assumes structures are mostly Mesozoic, either reactivated or preserved by late Cenozoic deformation. The main difference between the interpretative cross‐sections is the degree to which active structures link into basal detachment and high‐strain zones at depth." @default.
• W2080862693 created "2016-06-24" @default.
• W2080862693 creator A5016721953 @default.
• W2080862693 creator A5021384610 @default.
• W2080862693 creator A5041575793 @default.
• W2080862693 creator A5058061052 @default.
• W2080862693 creator A5083900265 @default.
• W2080862693 date "2003-03-01" @default.
• W2080862693 modified "2023-10-13" @default.
• W2080862693 title "Upper crustal structure beneath the eastern Southern Alps and the Mackenzie Basin, New Zealand, derived from seismic reflection data" @default.
• W2080862693 cites W1517589768 @default.
• W2080862693 cites W1829098717 @default.
• W2080862693 cites W1967687859 @default.
• W2080862693 cites W1969127085 @default.
• W2080862693 cites W1969505301 @default.
• W2080862693 cites W1970596376 @default.
• W2080862693 cites W1972964689 @default.
• W2080862693 cites W1974431677 @default.
• W2080862693 cites W1978319611 @default.
• W2080862693 cites W1983657909 @default.
• W2080862693 cites W1983900553 @default.
• W2080862693 cites W1993477842 @default.
• W2080862693 cites W1994328493 @default.
• W2080862693 cites W1998190601 @default.
• W2080862693 cites W2004918714 @default.
• W2080862693 cites W2006764344 @default.
• W2080862693 cites W2008179277 @default.
• W2080862693 cites W2008184529 @default.
• W2080862693 cites W2011148282 @default.
• W2080862693 cites W2011516386 @default.
• W2080862693 cites W2015012869 @default.
• W2080862693 cites W2016226173 @default.
• W2080862693 cites W2023065276 @default.
• W2080862693 cites W2023434032 @default.
• W2080862693 cites W2027005183 @default.
• W2080862693 cites W2028633980 @default.
• W2080862693 cites W2030393339 @default.
• W2080862693 cites W2030769971 @default.
• W2080862693 cites W2033354436 @default.
• W2080862693 cites W2035490756 @default.
• W2080862693 cites W2036915462 @default.
• W2080862693 cites W2037397108 @default.
• W2080862693 cites W2037859991 @default.
• W2080862693 cites W2039380582 @default.
• W2080862693 cites W2041276447 @default.
• W2080862693 cites W2043652106 @default.
• W2080862693 cites W2046025499 @default.
• W2080862693 cites W2047378493 @default.
• W2080862693 cites W2049386485 @default.
• W2080862693 cites W2049808999 @default.
• W2080862693 cites W2052090465 @default.
• W2080862693 cites W2053907214 @default.
• W2080862693 cites W2054770080 @default.
• W2080862693 cites W2054867889 @default.
• W2080862693 cites W2058131199 @default.
• W2080862693 cites W2059766962 @default.
• W2080862693 cites W2060378572 @default.
• W2080862693 cites W2081827640 @default.
• W2080862693 cites W2085576499 @default.
• W2080862693 cites W2085918114 @default.
• W2080862693 cites W2087840269 @default.
• W2080862693 cites W2090632481 @default.
• W2080862693 cites W2091018529 @default.
• W2080862693 cites W2092741644 @default.
• W2080862693 cites W2094173483 @default.
• W2080862693 cites W2095112561 @default.
• W2080862693 cites W2098626827 @default.
• W2080862693 cites W2099221032 @default.
• W2080862693 cites W2113148209 @default.
• W2080862693 cites W2117711986 @default.
• W2080862693 cites W2119059793 @default.
• W2080862693 cites W2124278013 @default.
• W2080862693 cites W2130468289 @default.
• W2080862693 cites W2133104066 @default.
• W2080862693 cites W2139584136 @default.
• W2080862693 cites W2141424304 @default.
• W2080862693 cites W2143597055 @default.
• W2080862693 cites W2143820619 @default.
• W2080862693 cites W2148272697 @default.
• W2080862693 cites W2152541268 @default.
• W2080862693 cites W2162496306 @default.
• W2080862693 cites W2168925255 @default.
• W2080862693 cites W2170225689 @default.
• W2080862693 cites W2332968052 @default.
• W2080862693 cites W4249648780 @default.
• W2080862693 doi "https://doi.org/10.1080/00288306.2003.9514993" @default.
• W2080862693 hasPublicationYear "2003" @default.
• W2080862693 type Work @default.
• W2080862693 sameAs 2080862693 @default.
• W2080862693 citedByCount "30" @default.
• W2080862693 countsByYear W20808626932012 @default.
• W2080862693 countsByYear W20808626932016 @default.
• W2080862693 countsByYear W20808626932017 @default.
• W2080862693 countsByYear W20808626932018 @default.
• W2080862693 crossrefType "journal-article" @default.
• W2080862693 hasAuthorship W2080862693A5016721953 @default.
• W2080862693 hasAuthorship W2080862693A5021384610 @default.
• W2080862693 hasAuthorship W2080862693A5041575793 @default.

• next