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Journal articles on the topic 'Geology Vanuatu'

Author: Grafiati

Published: 11 December 2022

Last updated: 31 July 2025

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1

Gunn, P. J., J. Mitchell, P. Pieters, and S. Temakon. "The Vanuatu Mineral Exploration Initiative." Exploration Geophysics 28, no. 1-2 (1997): 209–13. http://dx.doi.org/10.1071/eg997209.

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2

Meffre, Sebastien, and Anthony J. Crawford. "Collision tectonics in the New Hebrides arc (Vanuatu)." Island Arc 10, no. 1 (2001): 33–50. http://dx.doi.org/10.1046/j.1440-1738.2001.00292.x.

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3

WELLS, ALICE, and KJELL ARNE JOHANSON. "Micro-caddisfly faunas of Australia and the southwest Pacific (Trichoptera, Hydroptilidae)." Zoosymposia 10, no. 1 (2016): 439–50. http://dx.doi.org/10.11646/zoosymposia.10.1.41.

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Today's distributions of faunal groups reflect historic events—geological and evolutionary, as well as dispersals, extinctions and chance events. The extent to which each of these contributed to the hydroptilid faunas of mainland Australia, Tasmania, New Guinea, New Zealand, New Caledonia, Fiji and Vanuatu is explored by comparison of the faunal composition, geology and geography of Australia and these SW Pacific islands. Corroborative evidence is sought from other groups, flora as well as fauna.

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4

Heyworth, Z., K. M. Knesel, S. P. Turner, and R. J. Arculus. "Pb-isotopic evidence for rapid trench-parallel mantle flow beneath Vanuatu." Journal of the Geological Society 168, no. 1 (2011): 265–71. http://dx.doi.org/10.1144/0016-76492010-054.

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5

Kotra, K. K., S. Bathula, and E. Sami. "Delineation of Groundwater Salinity Zones in Shefa and Malampa Provinces, Vanuatu." Nature Environment and Pollution Technology 21, no. 2 (2022): 803–12. http://dx.doi.org/10.46488/nept.2022.v21i02.045.

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A preliminary assessment was carried out in identifying the salinity zones due to considerable concern over salty groundwater resources in Vanuatu’s Shefa and Malampa regions. Electrical conductivity (EC) and pH were measured on the islands of Efate, Lamen, and Nguna in Shefa province, as well as the islands of Ambrym and Paama in Malampa province. Thirty-four percent of the samples exceeded Vanuatu’s National Drinking Water Standards with an average of 3123 μS/Cm indicating possible salinity zones. Whereas the average pH of 7.21 was in the range of acceptable levels. EC values as high as 18,5

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6

Baillard, Christian, Wayne C. Crawford, Valérie Ballu, Bernard Pelletier, and Esline Garaebiti. "Tracking subducted ridges through intermediate-depth seismicity in the Vanuatu subduction zone." Geology 46, no. 9 (2018): 767–70. http://dx.doi.org/10.1130/g45010.1.

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7

McConachy, Timothy F., Richard J. Arculus, Christopher J. Yeats, et al. "New hydrothermal activity and alkalic volcanism in the backarc Coriolis Troughs, Vanuatu." Geology 33, no. 1 (2005): 61. http://dx.doi.org/10.1130/g20870.1.

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8

Hallwright, Joshua, and John Handmer. "Accountability and transparency in disaster aid: Cyclone Pam in Vanuatu." International Journal of Disaster Risk Reduction 36 (May 2019): 101104. http://dx.doi.org/10.1016/j.ijdrr.2019.101104.

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9

Jago, J., M. Pharaoh, and C. Wilson-Roberts. "Douglas Mawson's First Major Geological Expedition: The New Hebrides, 1903." Earth Sciences History 24, no. 1 (2005): 93–111. http://dx.doi.org/10.17704/eshi.24.1.f771465730u1w938.

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Douglas Mawson, the famous Australian geologist and Antarctic explorer, is best known for his Antarctic expeditionary work, first with Shackleton in 1907-09, and later in 1911-14 and 1929-31 on expeditions that he led himself. However, his first expedition outside of Australia was to the New Hebrides (modern Vanuatu) in 1903 at the age of 20 and before he had completed his geology degree. Mawson's field notes, and subsequent publications, are most impressive given that they were produced by a very young inexperienced geologist, working independently in an isolated area. His field notes and pho

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10

Niroa, John Junior, and Naohiro Nakamura. "Volcanic disaster risk reduction in indigenous communities on Tanna Island, Vanuatu." International Journal of Disaster Risk Reduction 74 (May 2022): 102937. http://dx.doi.org/10.1016/j.ijdrr.2022.102937.

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11

Neef, Gerrit, and Chris Hendy. "Late Pleistocene-Holocene Acceleration of Uplift Rate in Southwest Erromango Island, Southern Vanuatu, South Pacific: Relation to the Growth of the Vanuatuan Mid Sedimentary Basin." Journal of Geology 96, no. 4 (1988): 481–94. http://dx.doi.org/10.1086/629242.

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12

Dawes, Nathan, Richard C. Franklin, Lachlan McIver, and Jimmy Obed. "General and post-disaster mental health servicing in Vanuatu: A qualitative analysis." International Journal of Disaster Risk Reduction 40 (November 2019): 101256. http://dx.doi.org/10.1016/j.ijdrr.2019.101256.

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13

Nakada, Setsuya, Patrick Maillet, Marie-Claire Monjaret, Akihiko Fujinawa, and Tetsuro Urabe. "High-Na dacite from the Jean Charcot Trough (Vanuatu), Southwest Pacific." Marine Geology 116, no. 1-2 (1994): 197–213. http://dx.doi.org/10.1016/0025-3227(94)90176-7.

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14

Cabioch, Guy. "Postglacial reef development in the South-West Pacific: case studies from New Caledonia and Vanuatu." Sedimentary Geology 159, no. 1-2 (2003): 43–59. http://dx.doi.org/10.1016/s0037-0738(03)00094-0.

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15

Bath, A. H., W. G. Burgess, and J. N. Carney. "The chemistry and hydrology of thermal springs on efate, vanuatu, sw pacific." Geothermics 15, no. 3 (1986): 277–94. http://dx.doi.org/10.1016/0375-6505(86)90105-7.

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16

Collot, J., M. Patriat, R. Sutherland, et al. "Chapter 2 Geodynamics of the SW Pacific: a brief review and relations with New Caledonian geology." Geological Society, London, Memoirs 51, no. 1 (2020): 13–26. http://dx.doi.org/10.1144/m51-2018-5.

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AbstractThe SW Pacific region consists of a succession of ridges and basins that were created by the fragmentation of Gondwana and the evolution of subduction zones since Mesozoic times. This complex geodynamic evolution shaped the geology of New Caledonia, which lies in the northern part of the Zealandia continent. Alternative tectonic models have been postulated. Most models agree that New Caledonia was situated on an active plate margin of eastern Gondwana during the Mesozoic. Extension affected the region from the Late Cretaceous to the Paleocene and models for this period vary in the loca

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17

Chen, Jeffrey K., Frederick W. Taylor, R. Lawrence Edwards, Hai Cheng, and G. S. Burr. "Recent Emerged Reef Terraces of the Yenkahe Resurgent Block, Tanna, Vanuatu: Implications for Volcanic, Landslide and Tsunami Hazards." Journal of Geology 103, no. 5 (1995): 577–90. http://dx.doi.org/10.1086/629777.

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18

Robin, Claude, Jean-Philippe Eissen, and Michel Monzier. "Mafic pyroclastic flows at Santa Maria (Gaua) Volcano, Vanuatu: the caldera formation problem in mainly mafic island arc volcanoes." Terra Nova 7, no. 4 (1995): 436–43. http://dx.doi.org/10.1111/j.1365-3121.1995.tb00539.x.

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19

NEEF, G., I. R. PLIMER, and R. S. BOTTRILL. "Submarine-fan deposited sandstone and rudite in a mid-Cenozoic interarc basin in Maewo, Vanuatu (New Hebrides)." Sedimentology 32, no. 4 (1985): 519–42. http://dx.doi.org/10.1111/j.1365-3091.1985.tb00468.x.

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20

Maurizot, P., J. Collot, D. Cluzel, and M. Patriat. "Chapter 6 The Loyalty Islands and Ridge, New Caledonia." Geological Society, London, Memoirs 51, no. 1 (2020): 131–45. http://dx.doi.org/10.1144/m51-2017-24.

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AbstractThe Loyalty Ridge lies to the east and NE of the Norfolk Ridge. The three main Loyalty Islands (Maré, Lifou and Ouvéa) emerge from the ridge at the same latitude as Grande Terre. The islands are uniformly composed of carbonate deposits, except for Maré, where Middle Miocene intra-plate basalts and associated volcaniclastic rocks form restricted outcrops. Miocene rhodolith limestones constitute the bulk of the carbonate cover of the three islands. On Maré, these platform accumulations are locally topped by a dolomitic hardground, which, in turn, is covered by Pliocene–Pleistocene coral-

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21

Buys, Janrich, Carl Spandler, Robert J. Holm, and Simon W. Richards. "Remnants of ancient Australia in Vanuatu: Implications for crustal evolution in island arcs and tectonic development of the southwest Pacific." Geology 42, no. 11 (2014): 939–42. http://dx.doi.org/10.1130/g36155.1.

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22

Hong, Isabel, Jessica E. Pilarczyk, Benjamin P. Horton, et al. "Sedimentological characteristics of the 2015 Tropical Cyclone Pam overwash sediments from Vanuatu, South Pacific." Marine Geology 396 (February 2018): 205–14. http://dx.doi.org/10.1016/j.margeo.2017.05.011.

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23

REGNIER, MARC, STEVEN MORIS, AVI SHAPIRA, ALONA MALITZKY, and GRAHAM SHORTEN. "MICROZONATION OF THE EXPECTED SEISMIC SITE EFFECTS ACROSS PORT VILA, VANUATU." Journal of Earthquake Engineering 4, no. 2 (2000): 215–31. http://dx.doi.org/10.1080/13632460009350369.

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24

Németh, Károly, Shane J. Cronin, Robert B. Stewart, and Douglas Charley. "Intra- and extra-caldera volcaniclastic facies and geomorphic characteristics of a frequently active mafic island–arc volcano, Ambrym Island, Vanuatu." Sedimentary Geology 220, no. 3-4 (2009): 256–70. http://dx.doi.org/10.1016/j.sedgeo.2009.04.019.

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25

Picard, C., M. Monzier, J. P. Eissen, and C. Robin. "Concomitant evolution of tectonic environment and magma geochemistry, Ambrym volcano (Vanuatu, New Hebrides arc)." Geological Society, London, Special Publications 81, no. 1 (1994): 135–54. http://dx.doi.org/10.1144/gsl.sp.1994.081.01.08.

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26

Zielske, Susan, and Martin Haase. "When snails inform about geology: Pliocene emergence of islands of Vanuatu indicated by a radiation of truncatelloidean freshwater gastropods (Caenogastropoda: Tateidae)." Journal of Zoological Systematics and Evolutionary Research 52, no. 3 (2013): 217–36. http://dx.doi.org/10.1111/jzs.12053.

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27

Cabioch, Guy, Gilbert Camoin, Gregory E. Webb, et al. "Contribution of microbialites to the development of coral reefs during the last deglacial period: Case study from Vanuatu (South-West Pacific)." Sedimentary Geology 185, no. 3-4 (2006): 297–318. http://dx.doi.org/10.1016/j.sedgeo.2005.12.019.

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28

Nasemann, Philipp, Melanie Gault-Ringold, Claudine H. Stirling, Andrea Koschinsky, and Sylvia G. Sander. "Processes affecting the isotopic composition of dissolved iron in hydrothermal plumes: A case study from the Vanuatu back-arc." Chemical Geology 476 (January 2018): 70–84. http://dx.doi.org/10.1016/j.chemgeo.2017.11.005.

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29

Greene, H. Gary, and Neville F. Exon. "Acoustic stratigraphy and hydrothermal activity within Epi Submarine Caldera, Vanuatu, New Hebrides Arc." Geo-Marine Letters 8, no. 3 (1988): 121–29. http://dx.doi.org/10.1007/bf02326088.

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30

Rabier, Cécile, Yannick Anguy, Guy Cabioch, and Pierre Genthon. "Characterization of various stages of calcitization in Porites sp corals from uplifted reefs — Case studies from New Caledonia, Vanuatu, and Futuna (South-West Pacific)." Sedimentary Geology 211, no. 3-4 (2008): 73–86. http://dx.doi.org/10.1016/j.sedgeo.2008.08.005.

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31

Nabyl, A., J. Dorel, and M. Lardy. "A comparative study of low‐frequency seismic signals recorded at Stromboli volcano, Italy, and at Yasur volcano, Vanuatu." New Zealand Journal of Geology and Geophysics 40, no. 4 (1997): 549–58. http://dx.doi.org/10.1080/00288306.1997.9514783.

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32

Obzhirov, A. I. "Dissolved gases of the near-bottom water layer in the area of Epi island, Vanuatu." Geo-Marine Letters 12, no. 4 (1992): 232–35. http://dx.doi.org/10.1007/bf02091844.

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33

Cabioch, Guy, Kirsten A. Banks-Cutler, Warren J. Beck, et al. "Continuous reef growth during the last 23calkyr BP in a tectonically active zone (Vanuatu, SouthWest Pacific)." Quaternary Science Reviews 22, no. 15-17 (2003): 1771–86. http://dx.doi.org/10.1016/s0277-3791(03)00170-7.

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34

Németh, Károly, and Shane J. Cronin. "Volcanic craters, pit craters and high-level magma-feeding systems of a mafic island-arc volcano: Ambrym, Vanuatu, South Pacific." Geological Society, London, Special Publications 302, no. 1 (2008): 87–102. http://dx.doi.org/10.1144/sp302.6.

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35

Lecolle, J. F., J. E. Bokilo, and M. Bernat. "Soulèvement et tectonique de l'île d'Efaté (Vanuatu) arc insulaire des Nouvelles-Hébrides, au cours du Quaternaire récent. Datations de terrasses soulevées par la méthode." Marine Geology 94, no. 3 (1990): 251–70. http://dx.doi.org/10.1016/0025-3227(90)90072-r.

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36

Hamilton, Alison M., Elaine R. Klein, and Christopher C. Austin. "Biogeographic Breaks in Vanuatu, A Nascent Oceanic Archipelago." Pacific Science 64, no. 2 (2010): 149–59. https://doi.org/10.5281/zenodo.13483366.

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(Uploaded by Plazi for the Bat Literature Project) The study of distinct biogeographic demarcations has played a pivotal role in our understanding processes responsible for patterns of species distributions and, importantly, the role of geologic processes in promoting biotic diversification. Biogeographic barriers such as Wallace's line have been shown to be the result of old geologic processes shaping ancient faunal or floral diversification events. Based on distributions of birds, bats, reptiles, plants, and invertebrates we identify a distinct biogeographic disjunction in Vanuatu, a geologi

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37

Hamilton, Alison M., Elaine R. Klein, and Christopher C. Austin. "Biogeographic Breaks in Vanuatu, A Nascent Oceanic Archipelago." Pacific Science 64, no. 2 (2010): 149–59. https://doi.org/10.5281/zenodo.13483366.

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Abstract:

(Uploaded by Plazi for the Bat Literature Project) The study of distinct biogeographic demarcations has played a pivotal role in our understanding processes responsible for patterns of species distributions and, importantly, the role of geologic processes in promoting biotic diversification. Biogeographic barriers such as Wallace's line have been shown to be the result of old geologic processes shaping ancient faunal or floral diversification events. Based on distributions of birds, bats, reptiles, plants, and invertebrates we identify a distinct biogeographic disjunction in Vanuatu, a geologi

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38

Hamilton, Alison M., Elaine R. Klein, and Christopher C. Austin. "Biogeographic Breaks in Vanuatu, A Nascent Oceanic Archipelago." Pacific Science 64, no. 2 (2010): 149–59. https://doi.org/10.5281/zenodo.13483366.

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Abstract:

(Uploaded by Plazi for the Bat Literature Project) The study of distinct biogeographic demarcations has played a pivotal role in our understanding processes responsible for patterns of species distributions and, importantly, the role of geologic processes in promoting biotic diversification. Biogeographic barriers such as Wallace's line have been shown to be the result of old geologic processes shaping ancient faunal or floral diversification events. Based on distributions of birds, bats, reptiles, plants, and invertebrates we identify a distinct biogeographic disjunction in Vanuatu, a geologi

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39

Hamilton, Alison M., Elaine R. Klein, and Christopher C. Austin. "Biogeographic Breaks in Vanuatu, A Nascent Oceanic Archipelago." Pacific Science 64, no. 2 (2010): 149–59. https://doi.org/10.5281/zenodo.13483366.

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Abstract:

(Uploaded by Plazi for the Bat Literature Project) The study of distinct biogeographic demarcations has played a pivotal role in our understanding processes responsible for patterns of species distributions and, importantly, the role of geologic processes in promoting biotic diversification. Biogeographic barriers such as Wallace's line have been shown to be the result of old geologic processes shaping ancient faunal or floral diversification events. Based on distributions of birds, bats, reptiles, plants, and invertebrates we identify a distinct biogeographic disjunction in Vanuatu, a geologi

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40

Hamilton, Alison M., Elaine R. Klein, and Christopher C. Austin. "Biogeographic Breaks in Vanuatu, A Nascent Oceanic Archipelago." Pacific Science 64, no. 2 (2010): 149–59. https://doi.org/10.5281/zenodo.13483366.

Full text

Abstract:

(Uploaded by Plazi for the Bat Literature Project) The study of distinct biogeographic demarcations has played a pivotal role in our understanding processes responsible for patterns of species distributions and, importantly, the role of geologic processes in promoting biotic diversification. Biogeographic barriers such as Wallace's line have been shown to be the result of old geologic processes shaping ancient faunal or floral diversification events. Based on distributions of birds, bats, reptiles, plants, and invertebrates we identify a distinct biogeographic disjunction in Vanuatu, a geologi

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41

Dickinson, William R. "Petrography and geologic provenance of sand tempers in prehistoric potsherds from Fiji and Vanuatu, South Pacific." Geoarchaeology 16, no. 3 (2001): 275–322. http://dx.doi.org/10.1002/1520-6548(200103)16:3<275::aid-gea1005>3.0.co;2-e.

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42

Maksimenko, N. I., T. G. Shumilova, and V. V. Ulyashev. "Complex characteristics of suevites at the B. Vanuyta river (Kara astrobleme, Russia)." LITHOSPHERE (Russia) 23, no. 5 (2023): 844–67. http://dx.doi.org/10.24930/1681-9004-2023-23-5-844-867.

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Research subject. Suevites from the eastern sector of the Kara astrobleme, located in the basin of the Bolshaya Vanuyta river. Aim. To identify the suevitic type and to clarify the facial features of the suevites from the B. Vanuyta River. Materials. Hand-size samples of suevites collecteed in the basins of B. Vanuyta, Anaroga, Kara, and Sopchayu rivers, as well as samples of siltstones collected outside the Kara crater (rivers Halmeryu, Sayakha, Putyu, Anaroga and the creek Lavovyi). The samples were used for preparing polished thin sections and powder specimens for analytical works. Methods.

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43

Matoza, Robin S., Bernard A. Chouet, Arthur D. Jolly, et al. "High-rate very-long-period seismicity at Yasur volcano, Vanuatu: source mechanism and decoupling from surficial explosions and infrasound." Geophysical Journal International 230, no. 1 (2022): 392–426. http://dx.doi.org/10.1093/gji/ggab533.

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SUMMARY Yasur volcano, Vanuatu is a continuously active open-vent basaltic-andesite stratocone with persistent and long-lived eruptive activity. We present results from a seismo-acoustic field experiment at Yasur, providing locally dense broad-band seismic and infrasonic network coverage from 2016 July 27 to August 3. We corroborate our seismo-acoustic observations with coincident video data from cameras deployed at the crater and on an unoccupied aircraft system (UAS). The waveforms contain a profusion of signals reflecting Yasur’s rapidly occurring and persistent explosive activity. The typi

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44

B. Pointoise, P. Charvis, J. Y. Col. "Deep Structure of the North Aoba Intra-Arc Basin, Vanuatu: ABSTRACT." AAPG Bulletin 74 (1990). http://dx.doi.org/10.1306/20b223d7-170d-11d7-8645000102c1865d.

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45

RODD, J., and W. BARCLAY, South Pac. "Hydrocarbon Prospectivity of the Island Intra-Arc Basins of Vanuatu and Solomon Islands." AAPG Bulletin 76 (1992). http://dx.doi.org/10.1306/f4c8fdc2-1712-11d7-8645000102c1865d.

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46

Bubb, Jackie, and Loïc Le Dé. "Participation as a requirement: Towards more inclusion or further exclusion? The community disaster and climate change committees in Vanuatu as a case study." International Journal of Disaster Risk Reduction, April 2022, 102992. http://dx.doi.org/10.1016/j.ijdrr.2022.102992.

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47

GREENE, H. GARY, U.S. Geological Su. "An Intra-Arc Basin as a Potential Hydrocarbon Prospect--Recent Results of Ocean Drilling Project Leg 134 Drilling in the North Aoba Basin, Vanuatu." AAPG Bulletin 76 (1992). http://dx.doi.org/10.1306/f4c8faf2-1712-11d7-8645000102c1865d.

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48

Strandberg, Nichola A., David A. Sear, Peter G. Langdon, et al. "Island ecosystem responses to the Kuwae eruption and precipitation change over the last 1600 years, Efate, Vanuatu." Frontiers in Ecology and Evolution 11 (February 23, 2023). http://dx.doi.org/10.3389/fevo.2023.1087577.

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IntroductionIslands of the Southwest Pacific are exposed to geologic and climate-related disturbances that occur on a range of timescales and which probably affect, to varying degrees, their terrestrial ecosystems. Over the past ∼1100 years we know of two major events in the region: the Kuwae eruption which is thought to have occurred ∼500 cal. years BP and a shift to drier conditions which began ∼1100 cal. years BP.MethodsWe investigated terrestrial and lacustrine ecosystem responses to these events and also to a changing fire regime, likely human-caused, using a multi-proxy (C/N, charcoal, c

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