Log in

Relevant bibliographies by topics / Intrusions (Geology) New Zealand / Journal articles

Journal articles on the topic 'Intrusions (Geology) New Zealand'

To see the other types of publications on this topic, follow the link: Intrusions (Geology) New Zealand.

Author: Grafiati

Published: 10 December 2022

Last updated: 28 January 2023

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the top 50 journal articles for your research on the topic 'Intrusions (Geology) New Zealand.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Browse journal articles on a wide variety of disciplines and organise your bibliography correctly.

1

Spandler, Carl J., Stephen M. Eggins, Richard J. Arculus, and John A. Mavrogenes. "Using melt inclusions to determine parent-magma compositions of layered intrusions: Application to the Greenhills Complex (New Zealand), a platinum group minerals–bearing, island-arc intrusion." Geology 28, no. 11 (2000): 991. http://dx.doi.org/10.1130/0091-7613(2000)28<991:umitdp>2.0.co;2.

Full text

APA, Harvard, Vancouver, ISO, and other styles

2

Cole, R. P., J. D. L. White, D. B. Townsend, G. S. Leonard, and C. E. Conway. "Glaciovolcanic emplacement of an intermediate hydroclastic breccia-lobe complex during the penultimate glacial period (190–130 ka), Ruapehu volcano, New Zealand." GSA Bulletin 132, no. 9-10 (January 9, 2020): 1903–13. http://dx.doi.org/10.1130/b35297.1.

Full text

Abstract:

Abstract An intermediate-composition hydroclastic breccia deposit is exposed in the upper reaches of a deep glacial valley at Ruapehu volcano, New Zealand, indicating an ancient accumulation of water existed near the current summit area. Lobate intrusions within the deposit have variably fluidal and brecciated margins, and are inferred to have been intruded while the deposit was wet and unconsolidated. The tectonic setting, elevation of Ruapehu, and glacial evidence suggest that the deposit-forming eruption took place in meltwater produced from an ancient glacier. The breccia-lobe complex is inferred to have been emplaced at > 154 ± 12 ka, during the penultimate glacial period (190–130 ka) when Ruapehu’s glaciers were more extensive than today. This age is based on overlying radiometrically dated lava flows, and by correlation with a well-constrained geochemical stratigraphy for Ruapehu. Field relations indicate that the glacier was at least 150 m thick, and ubiquitous quench textures and jigsaw-fit fracturing suggest that the clastic deposit was formed from non-explosive fragmentation of lava in standing water. Such features are unusual for the high flanks of a volcanic edifice where steep topography typically hinders accumulation of water or thick ice, and hence the formation and retention of hydroclastic material. Although not well-constrained for this time, the vent configuration at Ruapehu is inferred to have contributed to an irregular edifice morphology, allowing thick ice to locally accumulate and meltwater to be trapped.

APA, Harvard, Vancouver, ISO, and other styles

3

Hopper, Derek J., and Ian E. M. Smith. "Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand." New Zealand Journal of Geology and Geophysics 39, no. 3 (September 1996): 389–402. http://dx.doi.org/10.1080/00288306.1996.9514721.

Full text

APA, Harvard, Vancouver, ISO, and other styles

4

Armstrong, P. A., P. J. J. Kamp, R. G. Allis, and D. S. Chapman. "Thermal effects of intrusion below the Taranaki Basin (New Zealand): evidence from combined apatite fission track age and vitrinite reflectance data." Basin Research 9, no. 2 (June 1997): 151–69. http://dx.doi.org/10.1046/j.1365-2117.1997.00039.x.

Full text

APA, Harvard, Vancouver, ISO, and other styles

5

Jongens, Richard, Andrew J. Tulloch, Terry L. Spell, Mark S. Rattenbury, John G. Begg, and Belinda Smith Lyttle. "Pember Diorite—an Early Jurassic intrusion in the Rakaia Terrane, Puketeraki Range, Canterbury, New Zealand." New Zealand Journal of Geology and Geophysics 52, no. 1 (March 2009): 37–42. http://dx.doi.org/10.1080/00288300909509876.

Full text

APA, Harvard, Vancouver, ISO, and other styles

6

Smith, Victoria C., Phil Shane, and Ian A. Nairn. "Reactivation of a rhyolitic magma body by new rhyolitic intrusion before the 15.8 ka Rotorua eruptive episode: implications for magma storage in the Okataina Volcanic Centre, New Zealand." Journal of the Geological Society 161, no. 5 (September 2004): 757–72. http://dx.doi.org/10.1144/0016-764903-092.

Full text

APA, Harvard, Vancouver, ISO, and other styles

7

Curtis, Michael L. "Palaeozoic to Mesozoic polyphase deformation of the Patuxent Range, Pensacola Mountains, Antarctica." Antarctic Science 14, no. 2 (June 2002): 175–83. http://dx.doi.org/10.1017/s0954102002000743.

Full text

Abstract:

The Patuxent Range forms the most southerly third of the Pensacola Mountains, East Antarctica. Largely unstudied since the original geological survey work of the 1960s, the Patuxent Range was thought to expose metasediments deformed by a single Precambrian event. However, new structural data collected from two geographically separate areas in the central Patuxent Range reveal the presence of three distinct generations of structures. A synthesis of the regional geology together with new data suggests that the Patuxent Formation was mildly deformed during end Cambrian times as part of the late stage Ross Orogeny. However, the most intense deformation, although poorly constrained in age, probably occurred during the Permo-Triassic Gondwanian Orogeny. A third phase of deformation predates the intrusion of 183 Ma lamprophyre dykes and involved an inferred vertical axis rotation of the pre-existing D1 and D2 structures and the localized development of a spaced foliation and mesoscale folding. These D3 structures may be the first evidence of an Early Jurassic deformation event in the Transantarctic Mountains, which correlates with the Peninsula and Rangitata I orogenies of the Antarctic Peninsula and New Zealand, respectively.

APA, Harvard, Vancouver, ISO, and other styles

8

Kutovaya, Anna, Karsten F. Kroeger, Hannu Seebeck, Stefan Back, and Ralf Littke. "Thermal Effects of Magmatism on Surrounding Sediments and Petroleum Systems in the Northern Offshore Taranaki Basin, New Zealand." Geosciences 9, no. 7 (June 29, 2019): 288. http://dx.doi.org/10.3390/geosciences9070288.

Full text

Abstract:

In the past two decades, numerical forward modeling of petroleum systems has been extensively used in exploration geology. However, modeling of petroleum systems influenced by magmatic activity has not been a common practice, because it is often associated with additional uncertainties and thus is a high risk associated with exploration. Subsurface processes associated with volcanic activity extensively influence all the elements of petroleum systems and may have positive and negative effects on hydrocarbon formation and accumulation. This study integrates 3D seismic data, geochemical and well data to build detailed 1D and 3D models of the Kora Volcano—a buried Miocene arc volcano in the northern Taranaki Basin, New Zealand. It examines the impact of magmatism on the source rock maturation and burial history in the northern Taranaki Basin. The Kora field contains a sub-commercial oil accumulation in volcanoclastic rocks that has been encountered by a well drilled on the flank of the volcano. By comparing the results of distinct models, we concluded that magmatic activity had a local effect on the thermal regime in the study area and resulted in rapid thermal maturation of the surrounding organic matter-rich sediments. Scenarios of the magmatic activity age (18, 11 and 8 Ma) show that the re-equilibration of the temperature after intrusion takes longer (up to 5 Ma) in the scenarios with a younger emplacement age (8 Ma) due to an added insulation effect of the thicker overburden. Results of the modeling also suggest that most hydrocarbons expelled from the source rock during this magmatic event escaped to the surface due to the absence of a proper seal rock at that time.

APA, Harvard, Vancouver, ISO, and other styles

9

Morley, C. K. "3-D seismic imaging of the plumbing system of the Kora Volcano, Taranaki Basin, New Zealand: The influence of syn-rift structure on shallow igneous intrusion architecture." Geosphere 14, no. 6 (October 24, 2018): 2533–84. http://dx.doi.org/10.1130/ges01645.1.

Full text

APA, Harvard, Vancouver, ISO, and other styles

10

Sutherland, Rupert, Philip Barnes, and Chris Uruski. "Miocene‐Recent deformation, surface elevation, and volcanic intrusion of the overriding plate during subduction initiation, offshore southern Fiordland, Puysegur margin, southwest New Zealand." New Zealand Journal of Geology and Geophysics 49, no. 1 (March 2006): 131–49. http://dx.doi.org/10.1080/00288306.2006.9515154.

Full text

APA, Harvard, Vancouver, ISO, and other styles

11

Bischoff, Alan Patrick, Andrew Nicol, and Mac Beggs. "Stratigraphy of architectural elements in a buried volcanic system and implications for hydrocarbon exploration." Interpretation 5, no. 3 (August 31, 2017): SK141—SK159. http://dx.doi.org/10.1190/int-2016-0201.1.

Full text

Abstract:

The interaction between magmatism and sedimentation creates a range of petroleum plays at different stratigraphic levels due to the emplacement and burial of volcanoes. This study characterizes the spatio-temporal distribution of the fundamental building blocks (i.e., architectural elements) of a buried volcano and enclosing sedimentary strata to provide insights for hydrocarbon exploration in volcanic systems. We use a large data set of wells and seismic reflection surveys from the offshore Taranaki Basin, New Zealand, compared with outcropping volcanic systems worldwide to demonstrate the local impacts of magmatism on the evolution of the host sedimentary basin and petroleum system. We discover the architecture of Kora volcano, a Miocene andesitic polygenetic stratovolcano that is currently buried by more than 1000 m of sedimentary strata and hosts a subcommercial discovery within volcanogenic deposits. The 22 individual architectural elements have been characterized within three main stratigraphic sequences of the Kora volcanic system. These sequences are referred to as premagmatic (predate magmatism), synmagmatic (defined by the occurrence of intrusive, eruptive, and sedimentary architectural elements), and postmagmatic (degradation and burial of the volcanic structures after magmatism ceased). Potential petroleum plays were identified based on the distribution of the architectural elements and on the geologic circumstances resulting from the interaction between magmatism and sedimentation. At the endogenous level, emplacement of magma forms structural traps, such as drag folds and strata jacked up above intrusions. At the exogenous level, syneruptive, intereruptive, and postmagmatic processes mainly form stratigraphic and paleogeomorphic traps, such as interbedded volcano-sedimentary deposits, and upturned pinchout of volcanogenic and nonvolcanogenic coarse-grained deposits onto the volcanic edifice. Potential reservoirs are located at systematic vertical and lateral distances from eruptive centers. We have determined that identifying the architectural elements of buried volcanoes is necessary for building predictive models and for derisking hydrocarbon exploration in sedimentary basins affected by magmatism.

APA, Harvard, Vancouver, ISO, and other styles

12

Campbell, Hamish, Alex Malahoff, Greg Browne, Ian Graham, and Rupert Sutherland. "New Zealand Geology." Episodes 35, no. 1 (March 1, 2012): 57–71. http://dx.doi.org/10.18814/epiiugs/2012/v35i1/006.

Full text

APA, Harvard, Vancouver, ISO, and other styles

13

BROWN, L. J., R. D. BEETHAM, B. R. PATERSON, and J. H. WEEBER. "Geology of Christchurch, New Zealand." Environmental & Engineering Geoscience I, no. 4 (December 1, 1995): 427–88. http://dx.doi.org/10.2113/gseegeosci.i.4.427.

Full text

APA, Harvard, Vancouver, ISO, and other styles

14

Weir, Graham J. "Heat output from spreading and rifting models of the Taupo Volcanic Zone, New Zealand." Journal of Applied Mathematics and Decision Sciences 5, no. 2 (January 1, 2001): 105–18. http://dx.doi.org/10.1155/s1173912601000098.

Full text

Abstract:

A conceptual model of the Taupo Volcanic Zone (TVZ) is developed, to a depth of 25 km, formed from three constant density layers. The upper layer is formed from eruption products. A constant rate of eruption is assumed, which eventually implies a constant rate of extension, and a constant rate of volumetric creation in the middle and bottom layers. Tectonic extension creates volume which can accomodate magmatic intrusions. Spreading models assume this volume is distributed throughout the whole region, perhaps in vertical dykes, whereas rifting models assume the upper crust is thinned and the volume created lies under this upper crust. Bounds on the heat flow from such magmatic intrusions are calculated. Heat flow calculations are performed and some examples are provided which match the present total heat output from the TVZ of about 4200 MW, but these either have extension rates greater than the low values of about 8 ± 4 mm/a being reported from GPS measurements, or else consider extension rates in the TVZ to have varied over time.

APA, Harvard, Vancouver, ISO, and other styles

15

Kurapov, Mikhail, Victoria Ershova, Andrei Khudoley, Marina Luchitskaya, Daniel Stockli, Alexander Makariev, Elena Makarieva, and Irina Vishnevskaya. "Latest Permian–Triassic magmatism of the Taimyr Peninsula: New evidence for a connection to the Siberian Traps large igneous province." Geosphere 17, no. 6 (November 5, 2021): 2062–77. http://dx.doi.org/10.1130/ges02421.1.

Full text

Abstract:

Abstract This study presents new whole rock major and trace element, Sr-Nd isotopic, petrographic, and geochronologic data for seven latest Permian (Changhsingian)–Late Triassic (Carnian) granitoid intrusions of the northwestern and northeastern Taimyr Peninsula in the Russian High Arctic. U-Pb zircon ages, obtained using secondary ion mass spectrometry (SIMS), sensitive high-resolution ion microprobe (SHRIMP), and laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS), define the crystallization age of the Taimyr intrusions studied as ranging from ca. 253 Ma to 228 Ma, which suggests two magmatic pulses of latest Permian–Early Triassic and Middle–Late Triassic age. Ar-Ar dating of biotite and amphibole indicate rapid cooling of the intrusions studied, but Ar-Ar ages of several samples were reset by secondary heating and hydrothermal activity induced by the Middle–Late Triassic magmatic pulse. Petrographic data distinguish two groups of granites: syenite–monzonites and granites–granodiorites. Sr-Nd isotopic data, obtained from the same intrusions, show a variation of initial (87Sr/86Sr)i ratios between 0.70377 and 0.70607, and εNd(t) values range between –6.9 and 1.2. We propose that the geochemical and isotopic compositions of the Late Permian–Triassic Taimyr granites record the existence of a magma mush zone that was generated by the two pulses of Siberian Traps large igneous province (LIP) magmatism.

APA, Harvard, Vancouver, ISO, and other styles

16

Bastin, Sarah H., Mark C. Quigley, and Kari Bassett. "Paleoliquefaction in Christchurch, New Zealand." Geological Society of America Bulletin 127, no. 9-10 (April 14, 2015): 1348–65. http://dx.doi.org/10.1130/b31174.1.

Full text

APA, Harvard, Vancouver, ISO, and other styles

17

Schmidt, Alexander R., Uwe Kaulfuss, Jennifer M. Bannister, Viktor Baranov, Christina Beimforde, Natalie Bleile, Art Borkent, et al. "Amber inclusions from New Zealand." Gondwana Research 56 (April 2018): 135–46. http://dx.doi.org/10.1016/j.gr.2017.12.003.

Full text

APA, Harvard, Vancouver, ISO, and other styles

18

Carter, Lionel, and I. Nicholas McCave. "Eastern New Zealand Drifts, Miocene-Recent." Geological Society, London, Memoirs 22, no. 1 (2002): 385–407. http://dx.doi.org/10.1144/gsl.mem.2002.022.01.27.

Full text

APA, Harvard, Vancouver, ISO, and other styles

19

Dickin, A. P. "Nd isotope chemistry of Tertiary igneous rocks from Arran, Scotland: implications for magma evolution and crustal structure." Geological Magazine 131, no. 3 (May 1994): 329–33. http://dx.doi.org/10.1017/s0016756800011092.

Full text

Abstract:

AbstractThe geochemistry of Tertiary igneous rocks from Arran, western Scotland, provides a probe for the structure of the crust in the region of the Highland Boundary Fault (HBF). New Nd isotope data, coupled with other geochemical evidence, point to variable contamination of primitive mantle-derived magmas during magmatic differentiation in the crust. Two different isotopic contamination trends are seen. The northern granite was generated by contamination of basic differentiates by crust resembling exposed Dalradian units. Data for the central granite, and several other minor intrusions from south of the HBF, trend towards the reported isotopic signatures of granulite-facies xenoliths from the Midland Valley. However, quartz porphyry intrusions in the south of the island are compositionally similar to the nothern granite, and were probably intruded southwards across the HBF in dykes. Hence the isotopic signatures of the Tertiary intrusions reflect the different character of the crustal units on either side of the fault.

APA, Harvard, Vancouver, ISO, and other styles

20

Lingen, G. J. "2. New Zealand Petroleum Conference: Rotorua, New Zealand." Journal of Petroleum Geology 17, no. 4 (October 1994): 483–84. http://dx.doi.org/10.1111/j.1747-5457.1994.tb00154.x.

Full text

APA, Harvard, Vancouver, ISO, and other styles

21

Fitzsimons, Sean, Michael Pollington, and Eric Colhoun. "Palaeomagnetism of New Zealand glacigenic deposits." Exploration Geophysics 24, no. 2 (June 1993): 303–4. http://dx.doi.org/10.1071/eg993303.

Full text

APA, Harvard, Vancouver, ISO, and other styles

22

de Lange, W. P., and V. G. Moon. "Tsunami washover deposits, Tawharanui, New Zealand." Sedimentary Geology 200, no. 3-4 (August 2007): 232–47. http://dx.doi.org/10.1016/j.sedgeo.2007.01.006.

Full text

APA, Harvard, Vancouver, ISO, and other styles

23

Hurst, Andrew, Antonio Grippa, Simone Y. Silcock, Mads Huuse, Mike Bowman, and Sarah L. Cobain. "Introduction: subsurface sand remobilization and injection." Geological Society, London, Special Publications 493, no. 1 (2021): 1–10. http://dx.doi.org/10.1144/sp493-2020-268.

Full text

Abstract:

AbstractObservation of basin-scale networks of sandstone intrusions are described from subsurface studies and outcrop locations. Regional scale studies are prevalent in the volume and two new regionally significant subsurface sand injection complexes are described. Higher resolution studies, both outcrop and subsurface, show the small-scale complexity but high level of connectedness of sandstone intrusions. Discordance with bedding at all scales is diagnostic of sandstone intrusions. The propensity of hydraulic fractures to develop and fill with fluidized sand in a broad range of host rocks is demonstrated by examples from metamorphic and magmatic basement, and lignite. Terminology used to describe sandstone intrusions and other elements of sand injection complexes is diverse.

APA, Harvard, Vancouver, ISO, and other styles

24

Zhang, Xuebing, Fengmei Chai, Chuan Chen, Hongyan Quan, and Xiaoping Gong. "Geochronology, geochemistry and tectonic implications of late Carboniferous Daheyan intrusions from the Bogda Mountains, eastern Tianshan." Geological Magazine 157, no. 2 (July 29, 2019): 289–306. http://dx.doi.org/10.1017/s001675681900075x.

Full text

Abstract:

AbstractThe Daheyan region, situated in the SW of the Bogda Mountains in eastern Tianshan, is important for understanding the accretionary history of the Central Asian Orogenic Belt. We investigated Carboniferous intrusions from the Daheyan area, SW Bogda Mountains, obtaining new zircon U–Pb ages, whole-rock geochemical data and Hf isotope data for these intrusions. Zircon U–Pb dating indicates that syenogranite, diorite, granodiorite and monzonite of the Daheyan intrusions were all formed during late Carboniferous (311–303 Ma) magmatism. The syenogranite has geochemical characteristics of A-type granites that were mainly sourced from melting of juvenile crust. In comparison, the low-Mg-number diorite intrusion, with tholeiite and metaluminous features, was derived from young crust and mixed some mantle materials. The granodiorite and monzonite are both I-type granites, and are both sourced from the melting of juvenile crust. Based on a comprehensive analysis of previous geochronological, geochemical and isotopic data of magmatic and sedimentary rocks in the Bogda–Harlik belt, we consider that late Carboniferous intrusive rocks of the Bogda Mountains formed in an intra-arc extension related to a continent-based arc setting.

APA, Harvard, Vancouver, ISO, and other styles

25

King, P. R., and P. H. Robinson. "An Overview of Taranaki Region Geology, New Zealand." Energy Exploration & Exploitation 6, no. 3 (June 1988): 213–32. http://dx.doi.org/10.1177/014459878800600304.

Full text

Abstract:

Recent revisions to the paleontologic dating and lithologic correlation of the late Cretaceous and Cenozoic sediments in many wells have improved the chronostratigraphic framework for the Taranaki Basin. When combined with detailed seismic mapping and results of a study of basement trends, refinements to the timing of major structural and sedimentary events in the basin's history can be made. A resultant series of paleogeographic maps is presented. The Taranaki Basin has developed primarily within an extensional tectonic regime, with a compressional overprint occurring variously in places from early Miocene to Pliocene. An overall transgressive sedimentary cycle existed from the late Cretaceous to early Miocene. Thereafter a generally regressive trend has continued to the present day. Subsidence patterns were broadly similar across the basin until the late Miocene, whereupon tectonic controls on basin morphology and sedimentation became more diverse.

APA, Harvard, Vancouver, ISO, and other styles

26

Bell, D. H., and J. R. Pettinga. "Engineering geology and subdivision planning in New Zealand." Engineering Geology 22, no. 1 (September 1985): 45–59. http://dx.doi.org/10.1016/0013-7952(85)90037-7.

Full text

APA, Harvard, Vancouver, ISO, and other styles

27

SEPPÄLÄ, MATTI. "A brief geology and palaeontology of New Zealand." Boreas 10, no. 4 (January 16, 2008): 368. http://dx.doi.org/10.1111/j.1502-3885.1981.tb00497.x.

Full text

APA, Harvard, Vancouver, ISO, and other styles

28

Wilson, C. J. N., V. R. Switsur, and A. P. Ward. "A new 14C age for the Oruanui (Wairakei) eruption, New Zealand." Geological Magazine 125, no. 3 (May 1988): 297–300. http://dx.doi.org/10.1017/s0016756800010232.

Full text

Abstract:

AbstractThe Oruanui eruption was the largest known outburst of Taupo volcano, New Zealand, and is among the larger Quaternary eruptions documented. The eruption deposits are variously known as the Oruanui, Wairakei, Kawakawa Tephra, or Aokautere Ash formations, and represent a bulk volume probably exceeding 500 km3. Four new 14C age determinations on carbonized vegetation in the non-welded Oruanui ignimbrite are combined to give a conventional age of 22590±230 yr b.p. Compared with the previously accepted figure of 20000 yr b.p., this new age resolves the anomaly of apparently older 14C ages being obtained from a demonstrably younger New Zealand deposit, and strengthens correlation of this eruption with an Antarctic ice-core acid anomaly. The trace of this eruption has great potential as a time-plane marker in the Antarctic just prior to the last glacial maximum. The close similarity in ages between the Oruanui and a comparable sized eruption (Ito/Aira-Tn) in Japan suggests that this period of activity may represent the best chance of resolving any linkages between large-scale explosive silicic volcanism and climate changes.

APA, Harvard, Vancouver, ISO, and other styles

29

Garnish, John. "11th New Zealand geothermal workshop." Geothermics 18, no. 5-6 (January 1989): 789–95. http://dx.doi.org/10.1016/0375-6505(89)90108-9.

Full text

APA, Harvard, Vancouver, ISO, and other styles

30

Low, Matthew. "The energetic cost of mate guarding is correlated with territorial intrusions in the New Zealand stitchbird." Behavioral Ecology 17, no. 2 (December 15, 2005): 270–76. http://dx.doi.org/10.1093/beheco/arj025.

Full text

APA, Harvard, Vancouver, ISO, and other styles

31

Gómez-Vasconcelos, Martha Gabriela, Pilar Villamor, Shane J. Cronin, Alan Palmer, Jonathan Procter, and Robert B. Stewart. "Spatio-temporal associations between dike intrusions and fault ruptures in the Tongariro Volcanic Center, New Zealand." Journal of Volcanology and Geothermal Research 404 (October 2020): 107037. http://dx.doi.org/10.1016/j.jvolgeores.2020.107037.

Full text

APA, Harvard, Vancouver, ISO, and other styles

32

Grapes, Rodney. "Geomorphology of faulting: The Wairarapa Fault, New Zealand." Zeitschrift für Geomorphologie Supplement Volumes 115 (July 1, 1999): 191–217. http://dx.doi.org/10.1127/zfgsuppl/115/1999/191.

Full text

APA, Harvard, Vancouver, ISO, and other styles

33

Dickson, Mark E., and Wayne J. Stephenson. "Chapter 13 The rock coast of New Zealand." Geological Society, London, Memoirs 40, no. 1 (2014): 225–34. http://dx.doi.org/10.1144/m40.13.

Full text

APA, Harvard, Vancouver, ISO, and other styles

34

Wadsworth, W. J. "Intraplate volcanism in Eastern Australia and New Zealand." Journal of Structural Geology 14, no. 3 (March 1992): 379–80. http://dx.doi.org/10.1016/0191-8141(92)90097-g.

Full text

APA, Harvard, Vancouver, ISO, and other styles

35

Ingham, M. R. "Geomagnetic induction studies in central New Zealand." Exploration Geophysics 17, no. 1 (March 1986): 35–36. http://dx.doi.org/10.1071/eg986035.

Full text

APA, Harvard, Vancouver, ISO, and other styles

36

McKnight, J. O., and F. H. Chamalaun. "A Magnetometer Array Experiment In New Zealand." Exploration Geophysics 24, no. 2 (June 1993): 191–94. http://dx.doi.org/10.1071/eg993191.

Full text

APA, Harvard, Vancouver, ISO, and other styles

37

McFadgen, B. G., and J. R. Goff. "Tsunamis in the New Zealand archaeological record." Sedimentary Geology 200, no. 3-4 (August 2007): 263–74. http://dx.doi.org/10.1016/j.sedgeo.2007.01.007.

Full text

APA, Harvard, Vancouver, ISO, and other styles

38

Goldsmith, P. R., and E. H. Smith. "Tunnelling soils in South Auckland, New Zealand." Engineering Geology 22, no. 1 (September 1985): 1–11. http://dx.doi.org/10.1016/0013-7952(85)90033-x.

Full text

APA, Harvard, Vancouver, ISO, and other styles

39

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 30, no. 4 (December 31, 1997): 371–72. http://dx.doi.org/10.5459/bnzsee.30.4.371-372.

Full text

APA, Harvard, Vancouver, ISO, and other styles

40

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 31, no. 1 (March 31, 1998): 69–70. http://dx.doi.org/10.5459/bnzsee.31.1.69-70.

Full text

APA, Harvard, Vancouver, ISO, and other styles

41

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 31, no. 3 (September 30, 1998): 213. http://dx.doi.org/10.5459/bnzsee.31.3.213.

Full text

APA, Harvard, Vancouver, ISO, and other styles

42

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 31, no. 4 (December 31, 1998): 298. http://dx.doi.org/10.5459/bnzsee.31.4.298.

Full text

APA, Harvard, Vancouver, ISO, and other styles

43

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 32, no. 1 (March 31, 1999): 41. http://dx.doi.org/10.5459/bnzsee.32.1.41.

Full text

APA, Harvard, Vancouver, ISO, and other styles

44

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 32, no. 2 (June 30, 1999): 123. http://dx.doi.org/10.5459/bnzsee.32.2.123.

Full text

APA, Harvard, Vancouver, ISO, and other styles

45

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 32, no. 3 (September 30, 1999): 190–91. http://dx.doi.org/10.5459/bnzsee.32.3.190-191.

Full text

APA, Harvard, Vancouver, ISO, and other styles

46

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 32, no. 4 (December 31, 1999): 263–64. http://dx.doi.org/10.5459/bnzsee.32.4.263-264.

Full text

APA, Harvard, Vancouver, ISO, and other styles

47

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 33, no. 1 (March 31, 2000): 60–61. http://dx.doi.org/10.5459/bnzsee.33.1.60-61.

Full text

APA, Harvard, Vancouver, ISO, and other styles

48

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 33, no. 2 (June 30, 2000): 173–74. http://dx.doi.org/10.5459/bnzsee.33.2.173-174.

Full text

APA, Harvard, Vancouver, ISO, and other styles

49

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 33, no. 4 (December 31, 2000): 498–500. http://dx.doi.org/10.5459/bnzsee.33.4.498-500.

Full text

APA, Harvard, Vancouver, ISO, and other styles

50

Editor. "Significant New Zealand earthquakes." Bulletin of the New Zealand Society for Earthquake Engineering 34, no. 1 (March 31, 2001): 87–89. http://dx.doi.org/10.5459/bnzsee.34.1.87-89.

Full text

APA, Harvard, Vancouver, ISO, and other styles

We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!