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Research Article

Petrology and crustal inheritance of the Cloudy Bay Volcanics as derived from a fluvial conglomerate, Papuan Peninsula (Papua New Guinea): An example of geological inquiry in the absence of in situ outcrop

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Article: 1450198 | Received 13 Jul 2017, Accepted 03 Mar 2018, Published online: 04 Apr 2018

References

  • Abers, G. A., & Roecker, S. W. (1991). Deep structure of an arc-continent collision: Earthquake relocation and inversion for upper mantle P and S wave velocities beneath Papua New Guinea. Journal of Geophysical Research: Solid Earth, 96, 6379–6401.10.1029/91JB00145
  • Adams, C. J., Cluzel, D., & Griffin, W. L. (2009). Detrital zircon ages and geochemistry of sedimentary rocks in basement Mesozoic terranes and their cover rocks in New Caledonia, and provenances at the Eastern Gondwanaland margin. Australian Journal of Earth Sciences, 56, 1023–1047.10.1080/08120090903246162
  • Ahrens, L. H., Cherry, R. D., & Erlank, A. J. (1967). Observations on the Th-U relationship in zircons from granitic rocks and from kimberlites. Geochemica et Cosmochimica Acta, 29, 711–716.
  • Amante, C., & Eakins, B. W. (2009). ETOPO1 1 arc-minute global relief model: Procedures, data sources and analysis. Silver Spring: NOAA Technical Memorandum NESDIS NGDC-24. National Geophysical Data Center, NOAA.
  • Ashley, P. M., & Flood, R. H. (1981). Low-K tholeiites and high-K igneous rocks from Woodlark Island, Papua New Guinea. Journal of the Geological Society of Australia, 28, 227–240.10.1080/00167618108729158
  • Australian Bureau of Mineral Resources. (1972). Geology of Papua NewGuinea, 1:1,000,000 map. Australian Bureau of Mineral Resources.
  • Baldwin, S. L., Fitzgerald, P. G., & Webb, L. E. (2012). Tectonics of the New Guinea Region. Annual Review of Earth and Planetary Sciences, 40, 495–520.10.1146/annurev-earth-040809-152540
  • Black, L. P., Kamo, S. L., Allen, C. M., Davis, D. W., Aleinikoff, J. N., Valley, J. W., … Foudoulis, C. (2004). Improved 206Pb/238U microprobe geochronology by the monitoring of trace-element-related matrix effect; SHRIMP, ID-TIMS, ELA-ICP-MS and oxygen isotope documentation for a series of zircon standards. Chemical Geology, 205, 115–140.10.1016/j.chemgeo.2004.01.003
  • Blewett, R. S., & Black, L. P. (1998). Structural and temporal framework of the Coen Region, north Queensland: Implications for major tectonothermal events in east and north Australia. Australian Journal of Earth Sciences, 45, 597–609.10.1080/08120099808728415
  • Buys, J., Spandler, C., Holm, R. J., & Richards, S. W. (2014). Remnants of ancient Australia in Vanuatu: Implications for crustal evolution in island arcs and tectonic development of the southwest Pacific. Geology, 42, 939–942.10.1130/G36155.1
  • Champion, D. C., & Bultitude, R. J. (2013). Kennedy igneous association. In P. A. Jell (Ed.), Geology of Queensland (pp. 473–514). Brisbane: Geological Survey of Queensland.
  • Chiaradia, M., Merino, D., & Spikings, R. (2009). Rapid transition to long-lived deep crustal magmatic maturation and the formation of giant porphyry-related mineralization (Yanacocha, Peru). Earth and Planetary Science Letters, 288, 505–515.10.1016/j.epsl.2009.10.012
  • Cloos, M., Sapiie, B., van Ufford, A. Q., Weiland, R. J., Warren, P. Q., & McMahon, T. P. (2005). Collisional delamination in New Guinea: The geotectonics of subducting slab breakoff (Special Paper, p. 400). Boulder: Geological Society of America.
  • Corfu, F., Hanchar, J. M., Hoskin, P. W. O., & Kinny, P. (2003). Atlas of zircon textures. In J. M. Hanchar & P. W. O. Hoskin (Eds.), Reviews in mineralogy & geochemistry 53: Zircon. Chantilly: Mineralogical Society of America.
  • Crowley, J. L., Schoene, B., & Bowring, S. A. (2007). U-Pb dating of zircon in the Bishop Tuff at the millennial scale. Geology, 35, 1123–1126.10.1130/G24017A.1
  • Davies, H. L. (2012). The geology of New Guinea—The cordilleran margin of the Australian continent. Episodes, 35, 87–102.
  • Davies, H. L., & Jaques, A. L. (1984). Emplacement of ophiolite in Papua New Guinea. Geological Society, London, Special Publications, 13, 341–349.10.1144/GSL.SP.1984.013.01.27
  • Davies, H. L., & Smith, I. E. (1971). Geology of Eastern Papua. Geological Society of America Bulletin, 82, 3299–3312.10.1130/0016-7606(1971)82[3299:GOEP]2.0.CO;2
  • Dow, D. B., Smit, J. A. J., Page, R. W. (1974). Wau–1:250,000 Geological Series. Explanatory notes to accompany Wau 1:250,000 geological map: Geological Survey of Papua New Guinea. Explanatory Notes SB/55-14.
  • Drummond, B. J., Collins, C. D. N., & Gibson, G. (1979). The crustal structure of the Gulf of Papua and north-west Coral Sea. BMR Australian Journal of Geology and Geophysics, 4, 341–351.
  • Eilon, Z., Abers, G. A., Gaherty, J. B., & Jin, G. (2015). Imaging continental breakup using telesiesmic body waves: The Woodlark Rift, Papua New Guinea. Geochemistry, Geophysics, Geosystems, 16, 2529–2548.10.1002/2015GC005835
  • Fergusson, C. L., Henderson, R. A., Fanning, C. M., & Withnall, I. W. (2007). Detrital zircon ages in Neoproterozoic to Ordovician siliciclastic rocks, northern Australia: Implications for the tectonic history of the East Gondwana continental margin. Journal of the Geological Society, 164, 215–225.10.1144/0016-76492005-136
  • Fergusson, C. L., Henderson, R. A., & Offler, R. (2017). Late Neoproterozoic to early Mesozoic sedimentary rocks of the Tasmanides, eastern Australia: Provenance switching associated with development of the East Gondwana active margin. In R. Mazumder (Ed.), Sediment Provenance (pp. 325–369). Netherlands: Elsevier.10.1016/B978-0-12-803386-9.00013-7
  • Fergusson, C. L., Henderson, R. A., Withnall, I. W., & Fanning, C. M. (2007). Structural history of the Greenvale Province, north Queensland: Early Palaeozoic extension and convergence on the Pacific margin of Gondwana. Australian Journal of Earth Sciences, 54, 573–595.10.1080/08120090701188970
  • Floyd, P. A., & Winchester, J. A. (1978). Identification and discrimination of altered and metamorphosed volcanic rocks using immobile elements. Chemical Geology, 21, 291–306.10.1016/0009-2541(78)90050-5
  • Gehrels, G. (2014). Detrital zircon U-Pb geochronology applied to tectonics. Annual Review of Earth and Planetary Sciences, 42, 127–149.10.1146/annurev-earth-050212-124012
  • Gill, J. B. (1981). Orogenic Andesites and plate tectonics. Berlin: Springer-Varlag.10.1007/978-3-642-68012-0
  • Graham, I. J., & Korsch, R. J. (1990). Age and provenance of granitoid clasts in Moeatoa Conglomerate, Kawhia Syncline, New Zealand. Journal of the Royal Society of New Zealand, 20, 25–39.10.1080/03036758.1990.10426731
  • Hall, R. (2002). Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: Computer-based reconstructions, model and animations. Journal of Asian Earth Sciences, 20, 353–431.10.1016/S1367-9120(01)00069-4
  • Heaman, L. M., Bowins, R., & Crocket, J. (1990). The chemical composition of igneous zircon suites: Implications for geochemical tracer studies. Geochimica et Cosmochimica Acta, 54, 1597–1607.10.1016/0016-7037(90)90394-Z
  • Henderson, R. A. (1986). Geology of the Mt Windsor subprovince—A lower Palaeozoic volcano-sedimentary terrane in the northern Tasman orogenic zone. Australian Journal of Earth Sciences, 33, 343–364.10.1080/08120098608729371
  • Hidaka, H., Shimizu, H., & Adachi, M. (2002). U-Pb geochronology and REE geochemistry of zircons from Palaeoproterozoic paragneiss clasts in the Mesozoic Kamiaso conglomerate, central Japan: Evidence for an Archean provenance. Chemical Geology, 187, 279–293.10.1016/S0009-2541(02)00058-X
  • Holm, R. J., Spandler, C., & Richards, S. W. (2013). Melanesian arc far-field response to collision of the Ontong Java Plateau: Geochronology and petrogenesis of the Simuku Igneous Complex, New Britain, Papua New Guinea. Tectonophysics, 603, 189–212.10.1016/j.tecto.2013.05.029
  • Holm, R. J., Spandler, C., & Richards, S. W. (2015). Continental collision, orogenesis and arc magmatism of the Miocene Maramuni arc, Papua New Guinea. Gondwana Research, 28, 1117–1136.10.1016/j.gr.2014.09.011
  • Holm, R. J., Rosenbaum, G., & Richards, S. W. (2016). Post 8 Ma reconstruction of Papua New Guinea and Solomon Islands: Microplate tectonics in a convergent plate boundary setting. Earth-Science Reviews, 156, 66–81.10.1016/j.earscirev.2016.03.005
  • Hoskin, P. W. O., & Schaltegger, U. (2003). The composition of zircon and igneous and metamorphic petrogenesis. In J. M. Hanchar & P. W. O. Hoskin (Eds.), Reviews in Mineralogy & Geochemistry 53: Zircon. Chantilly: Mineralogical Society of America.
  • Irvine, T. N., & Baragar, W. R. A. (1971). A guide to the chemical classification of the common volcanic rocks. Canadian Journal of Earth Sciences, 8, 523–548.10.1139/e71-055
  • Jackson, S. E., Pearson, N. J., Griffin, W. L., & Belousova, E. E. (2004). The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology. Chemical Geology, 211, 47–69.10.1016/j.chemgeo.2004.06.017
  • Jakeš, P., & Smith, I. E. M. (1970). High potassium calc-alkaline rocks from Cape Nelson, eastern Papua. Contributions to Mineralogy and Petrology, 28, 259–271.10.1007/BF00388948
  • Kemp, A. I. S., Hawkesworth, C. J., Collins, W. J., Gray, C. M., Blevin, P. L., & EIMF. (2009). Isotopic evidence for rapid continental growth in an extensional accretionary orogen: The Tasmanides, eastern Australia. Earth and Planetary Science Letters, 284, 455–466.10.1016/j.epsl.2009.05.011
  • Kennedy, A. K., Wotzlaw, J.-F., Schaltegger, U., Crowley, J. L., & Schmitz, M. (2014). Eocene zircon reference material for microanalysis of U-Th-Pb isotopes and trace elements. The Canadian Mineralogist, 52, 409–421.10.3749/canmin.52.3.409
  • Kopi, G., Findlay, R. H., & Williams, I. (2000). Age and provenance of the Owen Stanley Metamorphic Complex. East Papuan Composite Terrane, Papua New Guinea: Geological Survey of Papua New Guinea, Report . (unpublished).
  • Korsch, R. J., Adams, C. J., Black, L. P., Foster, D. A., Murray, C. G., Foudoulis, C., & Griffin, W. L. (2009). Geochronology and provenance of the Late Paleozoic accretionary wedge and Gympie Terrane, New England Orogen, eastern Australia. Australian Journal of Earth Sciences, 56, 655–685.10.1080/08120090902825776
  • Lamminen, J., Andersen, T., & Nystuen, J. P. (2015). Provenance and rift basin architecture of the Neoproterozoic Hedmark Basin, South Norway inferred from U-Pb ages and Lu-Hf isotopes of conglomerate clasts and detrital zircons. Geological Magazine, 152, 80–105.10.1017/S0016756814000144
  • Le Maitre, R. W. (Ed.). (2002). Igneous rocks: A classification and glossary of terms (2nd ed., pp. 236). Cambridge: Cambridge University Press.
  • Ludwig, K. R. (2009). User’s manual for isoplot 3.70: A geochronological toolkit for microsoft excel. Berkeley: Berkeley Geochronology Center Special Publication No. 4.
  • Lus, W. Y., McDougall, I., & Davies, H. L. (2004). Age of the metamorphic sole of the Papuan Ultramafic Belt ophiolite, Papua New Guinea. Tectonophysics, 392, 85–101.10.1016/j.tecto.2004.04.009
  • Macpherson, C. G., Dreher, S. T., & Thirlwall, M. F. (2006). Adakites without slab melting: High pressure differentiation of island arc magma, Mindanao, the Philippines. Earth and Planetary Science Letters, 243, 581–593.10.1016/j.epsl.2005.12.034
  • Milsom, J., & Smith, I. E. (1975). Southeastern Papua: Generation of thick crust in a tensional environment. Geology, 3, 117–120.10.1130/0091-7613(1975)3<117:SPGOTC>2.0.CO;2
  • Mortimer, N., Hauff, F., & Calvert, A. T. (2008). Continuation of the New England Orogen, Australia, beneath the Queensland Plateau and Lord Howe Rise. Australian Journal of Earth Sciences, 55, 195–209.10.1080/08120090701689365
  • Næraa, T., Scherstén, A., Rosing, M. T., Kemp, A. I. S., Hoffmann, J. E., Kokfelt, T. F., & Whitehouse, M. J. (2012). Hafnium isotope evidence for a transition in the dynamics of continental growth 3.2 Gyr ago. Nature, 485, 627–630.10.1038/nature11140
  • Ott, B., & Mann, P. (2015). Late Miocene to Recent formation of the Aure-Moresby fold-thrust belt and foreland basin as a consequence of Woodlark microplate rotation, Papua New Guinea. Geochemistry, Geophysics, Geosystems, 16, 1988–2004.10.1002/2014GC005668
  • Paquette, J.-L., & Le Pennec, J.-L. (2012). 3.8 Ga zircons sampled by Neogene ignimbrite eruptions in Central Anatolia. Geology, 40, 239–242.10.1130/G32472.1
  • Parrish, R. R. (1990). U-Pb dating of monazite and its application to geological problems. Canadian Journal of Earth Sciences, 27, 1431–1450.10.1139/e90-152
  • Peccerillo, A., & Taylor, S. R. (1976). Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey. Contributions to Mineralology and Petrology, 58, 68–81.
  • Pell, S. D., Williams, I. S., & Chivas, A. R. (1997). The use of protolith zircon-age fingerprints in determining the protosource areas for some Australian dune sands. Sedimentary Geology, 109, 233–260.10.1016/S0037-0738(96)00061-9
  • Pieters, P. E. (1978). Port Moresby-Kalo-Aroa, Papua New Guinea - 1:250 000 Geological Map Series (p. 55). BMR Australia Explanatory Notes.
  • Pirard, C., & Spandler, C. (2017). The zircon record of high-pressure metasedimentary rocks of New Caledonia: Implications for regional tectonics of the south-west Pacific. Gondwana Research, 46, 79–94.10.1016/j.gr.2017.03.001
  • Samuel, M. D., Be’eri-Shlevin, Y., Azer, M. K., Whitehouse, M. J., & Moussa, H. E. (2011). Provenance of conglomerate clasts from the volcano-sedimentary sequence at Wadi Rutig in southern Sinai, Egypt as revealed by SIMS U-Pb dating of zircon. Gondwana Research, 20, 450–464.10.1016/j.gr.2010.11.021
  • Schärer, U. (1984). The effect of initial 230Th disequilibrium on young U-Pb ages: The Makalu case, Himalaya. Earth and Planetary Science Letters, 67, 191–204.10.1016/0012-821X(84)90114-6
  • Schellart, W. P., Lister, G. S., & Toy, V. G. (2006). A late cretaceous and Cenozoic reconstruction of the Southwest Pacific region: Tectonics controlled by subduction and slab rollback processes. Earth-Science Reviews, 76, 191–233.10.1016/j.earscirev.2006.01.002
  • Schott, R. C., & Johnson, C. M. (2001). Garnet-bearing trondhjemite and other conglomerate clasts from the Gualala basin, California: Sedimentary record of the missing western portion of the Salinian magmatic arc? Geological Society of America Bulletin, 113, 870–880.10.1130/0016-7606(2001)113<0870:GBTAOC>2.0.CO;2
  • Shaanan, U., Rosenbaum, G., Hoy, D., & Mortimer, N. (2018). Late Paleozoic geology of the Queensland Plateau (offshore northeastern Australia). Australian Journal of Earth Sciences. doi:10.1080/08120099.2018.1426041
  • Shearman, P., & Bryan, J. (2011). A bioregional analysis of the distribution of rainforest cover, deforestation and degradation in Papua New Guinea. Austral Ecology, 36, 9–24.10.1111/aec.2011.36.issue-1
  • Shearman, P. L., Ash, J., Mackey, B., Bryan, J. E., & Lokes, B. (2009). Forest conversion and degradation in Papua New Guinea 1972–2002. Biotropica, 41, 379–390.10.1111/btp.2009.41.issue-3
  • Smith, I. E. (1972). High-potassium intrusives from southeastern Papua. Contributions to Mineralogy and Petrology, 34, 167–176.10.1007/BF00373771
  • Smith, I. E. M. (1976). Volcanic rocks from southeastern Papua: The Evolution of volcanism at a plate boundary ( Unpublished PhD Thesis, p. 298). Canberra: Australian National University.
  • Smith, I. E. (1982). Volcanic evolution in eastern Papua. Tectonophysics, 87, 315–333.10.1016/0040-1951(82)90231-1
  • Smith, I. E. M. (2013a). The chemical characterization and tectonic significance of ophiolite terrains in southeastern Papua New Guinea. Tectonics, 32, 1–12.
  • Smith, I. E. M. (2013b). High-magnesium andesites: The example of the Papuan Volcanic Arc. In A. Gómez-Tuena, S. M. Straub, & G. F. Zellmer (Eds.), Orogenic andesites and crustal growth (p. 385). London: Geological Society, Special Publications.
  • Smith, I. E., & Davies, H. L. (1976). Geology of the southeast Papuan mainland. BMR Journal of Australian Geology and Geophysics, 165, 86p.
  • Smith, I. E., & Milsom, J. S. (1984). Late Cenozoic volcanism and extension in Eastern Papua. Geological Society, London, Special Publications, 16, 163–171.10.1144/GSL.SP.1984.016.01.12
  • Stacey, J. S., & Kramers, J. D. (1975). Approximation of terrestrial lead isotope evolution by a two-stage model. Earth and Planetary Science Letters, 26, 207–221.10.1016/0012-821X(75)90088-6
  • Sun, S., & McDonough, W. F. (1989). Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. Geological Society, London, Special Publications, 42, 313–345.10.1144/GSL.SP.1989.042.01.19
  • Tapster, S., Roberts, N. M. W., Petterson, M. G., Saunders, A. D., & Naden, J. (2014). From continent to intra-oceanic arc: Zircon xenocrysts record the crustal evolution of the Solomon island arc. Geology, 42, 1087–1090.10.1130/G36033.1
  • Taylor, B., Goodliffe, A., Martinez, F., & Hey, R. (1995). Continental rifting and initial sea-floor spreading in the Woodlark basin. Nature, 374, 534–537.10.1038/374534a0
  • Taylor, B., Goodliffe, A. M., & Martinez, F. (1999). How continents break up: Insights from Papua New Guinea. Journal of Geophysical Research: Solid Earth, 104, 7497–7512.10.1029/1998JB900115
  • Tera, F., & Wasserburg, G. J. (1972). U-Th-Pb systematics in three Apollo 14 basalts and the problem of initial Pb in lunar rocks. Earth and Planetary Science Letters, 14, 281–304.10.1016/0012-821X(72)90128-8
  • Van Achterbergh, E., Ryan, C. G., Jackson, S. E., Griffin, W. L. (2001). Appendix. In P. J. Sylvester (Ed.), Laser Ablation-ICP-Mass Spectrometry in the Earth Sciences: Principle and Applications (Vol. 29, p. 239). Ottawa, ON: Mineralog. Assoc. Can. (MAC) Short Course Series.
  • Van Wyck, N., & Williams, I. S. (2002). Age and provenance of basement metasediments from the Kubor and Bena Bena Blocks, central Highlands, Papua New Guinea: Constraints on the tectonic evolution of the northern Australian cratonic margin. Australian Journal of Earth Sciences, 49, 565–577.10.1046/j.1440-0952.2002.00938.x
  • Wallace, L. M., Ellis, S., Little, T., Tregoning, P., Palmer, N., Rosa, R., … Kwazi, J. (2014). Continental breakup and UHP rock exhumation in action: GPS results from the Woodlark Rift, Papua New Guinea. Geochemistry, Geophysics, Geosystems, 15, 4267–4290.10.1002/2014GC005458
  • Wandres, A. M., Bradshaw, J. D., Weaver, S., Maas, R., Ireland, T., & Eby, N. (2004). Provenance analysis using conglomerate clast lithologies: A case study from the Pahau terrane of New Zealand. Sedimentary Geology, 167, 57–89.10.1016/j.sedgeo.2004.02.002
  • Webb, L. E., Baldwin, S. L., & Fitzgerald, P. G. (2014). The early-middle miocene subduction complex of the louisiade archipelago, southern margin of the woodlark rift. Geochemistry, Geophysics, Geosystems, 15, 4024–4046.10.1002/2014GC005500
  • Whattam, S. A., Malpas, J., Ali, J. R., & Smith, I. E. M. (2008). New SW Pacific tectonic model: Cyclical intraoceanic magmatic arc construction and near-coeval emplacement along the Australia-Pacific margin in the Cenozoic. Geochemistry, Geophysics, Geosystems, 9, Q03021.
  • Worthing, M. A., & Crawford, A. J. (1996). The igneous geochemistry and tectonic setting of metabasites from the Emo Metamorphics, Papua New Guinea; a record of the evolution and destruction of a backarc basin. Mineralogy and Petrology, 58, 79–100.10.1007/BF01165765