... some of these plutonic sources were exposed at the time of deposition of the Mount Somers quartz arenites. These sources were located to the WSW of the Mount Somers area during the Eocene, before onset of major displacement of the Karamea and Hohonu batholiths along the Alpine Fault since the Miocene...

... Zealand is part of the Australian Plate, which is bounded to the east by the Alpine Fault (Wellman, 1955 ) ( Fig. 2 ). High-grade gneisses and granitoids are exposed in the Paparoa, Victoria and Hohonu ranges (Tulloch & Kimbrough, 1989 ), the Fraser Complex, wedged between the Fraser and Alpine...

... are from Hohshu arc; 3 is from Kamchatka. Figure 3. Heavy line shows inferred crustal thickness variation with time, New Zealand orogen, based on the maximum Ce/Y values in basaltic suites. Dark shaded regions are crustal thickening periods; light regions are extensional periods. HD—Hohonu Dike...

... primitive, weakly adakitic, slab-derived lavas. The 97 Ma A-type granites and a basalt from the easternmost Chatham Rise enlarge the known area of postsubduction Gondwana magmatism. Amphibolite-grade schists from a fault block south of the Chatham Rise provide a critical bridge between the Zealandia...

... this applies are the Akatore, Dunstan, Kina, Inglewood, Oaonui, Pihama, Hohonu, and Titri faults (Fig.  3 ); and these steps produced a 1D PDF of MRI for each paleoseismologic site based on earthquake timings. For use in the NZ NSHM 2022, the mode of this PDF is output along with its 2.275%, 15.865%, 84.135...

...Figure 3. Simplified geologic and geomorphic map of the Inchbonnie area (modified after Nathan et al., 2002 ). The Alpine fault is shown from left to right. Holocene alluvial surfaces are shown in white. In this area the Pacific plate is composed of a sequence of regionally metamorphosed...

... characteristics, petrography and geochronology of the Hohonu Batholith and adjacent Granite Hill Complex, North Westland, New Zealand New Zealand Journal of Geology and Geophysics 1997 40 1 17 Whalen J.B. Currie K.L. Chappell B.W. A-type granites: geochemical characteristics...

...., Sircombe & Kamp 1998 ) and to the southeast by the Southern Alps mountain belt. This belt belongs to the Wakatipu Metamorphic Belt (WMB) in the Eastern Province of South Island. Both metamorphic belts are divided by the Alpine Fault, positioned about 20 km southeast of Gillespie’s Beach. South Island...

... with the fold-parallel Oriental shear zone, with the Globe-Progress shear zone acting as a tear fault that transferred contractional deformation on the Oriental shear zone across the structural grain of the adjacent folded rocks, during or soon after the end of greenschist facies metamorphism. An early phase...

... Province of New Zealand is recognized in several granitoid suites. The Separation Point and Hohonu Batholiths have prolonged geological histories dating back to the Paleozoic, but with the main construction taking place during the mid-Cretaceous ( Muir et al., 1994 ; Waight et al., 1997 ). The plutons...

... and crustal growth via slab melting: Archean to modern comparisons Journal of Geophysical Research 1990 95B 21503 21521 Gibson G.M. Late Mesozoic crustal Structure of Fiordland: legacy of regional thrust faulting or extensional collapse Geological Society of New Zealand Miscellaneous...

... of the Pelly Mountains within the Quiet Lake map sheet (NTS 105F) south of the Tintina Fault. Inset shows the general location within Yukon Territory. Teeth on thrust faults indicate the upper plate. The rectangle corresponds to the area shown in Figure 2 . Data plotted using UTM Zone 9N and NAD83. F...

... above a basement terrane boundary represented by the Livingstone Fault; the recently active Auckland Volcanic Field is similarly located along-strike on North Island. We suggest that the Livingstone Fault controlled the location of the Tuatara Volcanic Field by producing relief at the base...

... (Fig. 1 ). A more extensive, western, ‘Buller’ terrane, comprises extensive quartzose turbiditic greywacke-dominated successions of Early Ordovician age, intruded by Carboniferous to Late Devonian (Karamea Batholith) and Cretaceous (Paparoa, Hohonu batholiths) granitoids. The smaller, eastern ‘Takaka...

... ). This complex relationship between the Otago Schist and Alpine Schist may account for the partial overlap of the compositional fields ( Fig. 4C ). To complicate the Alpine Schist compositional field further, Higham (1996) and Cooper and Norris (2011) have shown that the mylonite of the Alpine fault zone...

... of Eastern Province sediment to the East Coast Basin. A long-lived sediment conduit that transported extraregional Western Province detritus to the south-central East Coast Basin may have developed along a structural precursor to the Alpine Fault. Marked Neogene increase of Upper Jurassic–Lower Cretaceous...

... the Alpine Fault, this region was adjacent to the SW margin of the Campbell Plateau. Similarly, pre-Neogene Taranaki and Western Southland basins would formerly have been adjacent. The oldest sedimentary rocks of the Zealandia Megasequence are Albian, Momotu Supergroup terrestrial sandstones...

..., located in the eastern fragment of the Qinling-Dabie orogen, originated from the Late Triassic collision between the Yangtze block and North China block ( Fig. 1 ). The orogenic belts are connected by the Minggang-Gushi fault to the north and the Xiangfan-Guangji fault to the south. The Gui-Mei fault...

... of South Island and Stewart Island (Western Province; Landis and Coombs, 1967 ; Tulloch, 1983 ) within the Buller and Takaka terranes ( Bishop et al., 1985 ; Cooper and Tulloch, 1992 ; Rattenbury et al., 1998 ; Jongens, 2006 ; Fig. 1 ). Miocene–Holocene movement on the Alpine fault has split...