Relevant bibliographies by topics / Basalte – Indien, Océan

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Academic literature on the topic 'Basalte – Indien, Océan'

Author: Grafiati
Published: 4 June 2021
Last updated: 17 February 2022

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Journal articles on the topic "Basalte – Indien, Océan"

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Fryer, Brian J., and John D. Greenough. "Evidence for mantle heterogeneity from platinum-group-element abundances in Indian Ocean basalts." Canadian Journal of Earth Sciences 29, no. 11 (1992): 2329–40. http://dx.doi.org/10.1139/e92-181.

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Oceanic-island tholeiitic basalts recovered from four sunken oceanic islands along the Reunion hot-spot trace show trace-element and mineralogical characteristics ranging from typical oceanic-island tholeiites to incompatible-element-depleted tholeiites resembling mid-ocean-ridge basalts. There are also variable degrees of magma evolution at each island. Noble metal (Au, Pd, Pt, Rh, Ru, Ir) abundances tend to decrease with magma evolution and with magma "alkalinity", indicating that the metals behave as compatible elements during crystal fractionation processes and during mantle melting proces
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RAY, DWIJESH, SAUMITRA MISRA, RANADIP BANERJEE, and DOMINIQUE WEIS. "Geochemical implications of gabbro from the slow-spreading Northern Central Indian Ocean Ridge, Indian Ocean." Geological Magazine 148, no. 3 (2010): 404–22. http://dx.doi.org/10.1017/s001675681000083x.

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AbstractGabbro samples (c. < 0.4 Ma old) dredged from close to the ‘Vityaz Megamullion’ on the slow-spreading Northern Central Indian Ridge (NCIR, 18–22 mm yr−1) include mostly olivine gabbro and Fe–Ti oxide gabbro. The cumulate olivine gabbro shows ophitic to subophitic texture with early formed plagioclase crystals in mutual contact with each other, and a narrow range of compositions of olivine (Fo80–81), clinopyroxene (magnesium number: 85–87) and plagioclase (An67–70). This olivine gabbro could be geochemically cogenetic with the evolved oxide gabbro. These gabbro samples are geochemica
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Maciąg, Łukasz, Dominik Zawadzki, Gabriela A. Kozub-Budzyń, Adam Piestrzyński, Ryszard A. Kotliński, and Rafał J. Wróbel. "Mineralogy of Cobalt-Rich Ferromanganese Crusts from the Perth Abyssal Plain (E Indian Ocean)." Minerals 9, no. 2 (2019): 84. http://dx.doi.org/10.3390/min9020084.

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Mineralogy of phosphatized and zeolitized hydrogenous cobalt-rich ferromanganese crusts from Dirck Hartog Ridge (DHR), the Perth Abyssal Plain (PAP), formed on an altered basaltic substrate, is described. Detail studies of crusts were conducted using optical transmitted light microscopy, X-ray Powder Diffraction (XRD) and Energy Dispersive X-ray Fluorescence (EDXRF), Differential Thermal Analysis (DTA) and Electron Probe Microanalysis (EPMA). The major Fe-Mn mineral phases that form DHR crusts are low-crystalline vernadite, asbolane and a feroxyhyte-ferrihydrite mixture. Accessory minerals are
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Seifert, Karl E., Melanie R. W. Cole, and Dale A. Brunotte. "REE mobility due to alteration of Indian Ocean basalt." Canadian Journal of Earth Sciences 22, no. 12 (1985): 1884–87. http://dx.doi.org/10.1139/e85-201.

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Indian Ocean basalts from DSDP site 249 on the Mozambique Ridge exhibit a progressive up-hole increase in alteration and Fe2O3/FeO and decrease in MgO and density over the approximately 3.5 m of recovered core. Abrupt increases in H2O+ and K2O and a decrease in CaO relative to lower basalt samples occur in the uppermost sample. These up-hole changes are accompanied by increasing REE and LREE/HREE and the development of a pronounced negative Ce anomaly. A rough estimate of the magnitude of chemical change is obtained by holding our most immobile element (Lu) constant.
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Hoareau, Jean-Luc, Eric Nicolini, Bertrand Fritz, and Eric Delcher. "Geochemical signatures of underground waters in a basaltic tropical environment. Experimental approach." Bulletin de la Société Géologique de France 176, no. 3 (2005): 257–67. http://dx.doi.org/10.2113/176.3.257.

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Abstract Introduction The Reunion Island is an oceanic basaltic island (2500 km2) located in the Indian Ocean under tropical climate (fig. 1). It comprises two shield volcanoes (i) the Piton des Neiges (3069 m omsl), active between 2.1 Ma and 12,000 y and now inactive; (ii) the Piton de la Fournaise (2631 m omsl), active still 1 Ma. This volcanic system presents the complete alkaline magmatic series from the most alkaline end-members to the most differentiate ones: oceanite, aphyric basalt, cotectic basalt, zeolitic basalt, plagioclase-rich basalt and mugearite (fig. 2). The humid climate, wit
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Renac, Christophe, Kurtis Kyser, Peter Bowden, Bertrand Moine, and Jean-Yves Cottin. "Hydrothermal fluid interaction in basaltic lava units, Kerguelen Archipelago (SW Indian Ocean)." European Journal of Mineralogy 22, no. 2 (2010): 215–34. http://dx.doi.org/10.1127/0935-1221/2009/0022-1993.

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Kiernan, Kevin, Anne McConnell, and Tony Yates. "Tube-fed pahoehoe lava-flow features of Azorella Peninsula, Heard Island, southern Indian Ocean." Polar Record 34, no. 190 (1998): 225–36. http://dx.doi.org/10.1017/s0032247400025699.

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AbstractAzorella Peninsula on Heard Island in the sub-Antarctic comprises basaltic scoria that is overlain by basalt flows. Typical tube-fed pahoehoe flows characteristic of some Hawaiian-type volcanoes occur. The volcanic landforms of the peninsula include highly degraded volcano remnants and undissected scoria cones, pahoehoe flows, lava rises, tumuli, open vertical volcanic conduits, and lava tubes. Features produced by lava inflation are widespread but are generally of low topographic relief. Many detailed lava-flow features are preserved in dramatically fresh condition within the protecte
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Brooks, C. Kent. "The East Greenland rifted volcanic margin." Geological Survey of Denmark and Greenland (GEUS) Bulletin 24 (December 22, 2011): 1–96. http://dx.doi.org/10.34194/geusb.v24.4732.

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The Palaeogene North Atlantic Igneous Province is among the largest igneous provinces in the world and this review of the East Greenland sector includes large amounts of information amassed since previous reviews around 1990.
 The main area of igneous rocks extends from Kangerlussuaq (c. 67°N) to Scoresby Sund (c. 70°N), where basalts extend over c. 65 000 km2 , with a second area from Hold with Hope (c. 73°N) to Shannon (c. 75°N). In addition, the Ocean Drilling Project penetrated basalt at five sites off South-East Greenland. Up to 7 km thickness of basaltic lavas have been stratigraphi
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Price, R. C., A. K. Kennedy, M. Riggs-Sneeringer, and F. A. Frey. "Geochemistry of basalts from the Indian Ocean triple junction: implications for the generation and evolution of Indian Ocean ridge basalts." Earth and Planetary Science Letters 78, no. 4 (1986): 379–96. http://dx.doi.org/10.1016/0012-821x(86)90005-1.

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Ahmad, Mansoor, Abdul Qayoom Paul, Priyanka Negi, Salim Akhtar, Bibhuti Gogoi, and Ashima Saikia. "Mafic rocks with back-arc E-MORB affinity from the Chotanagpur Granite Gneiss Complex of India: relicts of a Proterozoic Ophiolite suite." Geological Magazine 158, no. 9 (2021): 1527–42. http://dx.doi.org/10.1017/s0016756821000078.

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AbstractThe Proterozoic Chotanagpur Granite Gneiss Complex (CGGC) at the northern boundary of the Central Indian Tectonic Zone (CITZ) of the eastern Indian shield preserves relics of fossilized oceanic back-arc crust. We describe the field, petrographical and geochemical characteristics of the mafic rocks comprising pillow basalts and dolerites from the Bathani area of the northern fringe of the CGGC, eastern India. The basalts consist of plagioclase feldspar, hornblende, opaque minerals (Fe–Ti oxide) and chlorite, and the dolerite consists of plagioclase, hornblende and opaque minerals. Our d
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Dissertations / Theses on the topic "Basalte – Indien, Océan"

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Meyzen, Christine. "Pétrogenèse des MORB dans les zones froides du manteau supérieur indien : la ride sud-ouest indienne et la discordance australo-antarctique." Vandoeuvre-les-Nancy, INPL, 2002. http://www.theses.fr/2002INPL019N.

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La ride sud-ouest indienne (SWIR) est une des rides les plus lentes (taux d'expansion : 1. 6 cm. An(-¹)) et les plus profondes du réseau mondial de rides médio-océaniques. La mission EDUL a permis d'échantillonner des verres basaltiques localisés entre 69°E, près du point triple de Rodriguez et de 49°E, à 300 km de la zone de fracture Gallieni. Les compositions géochimiques des verres basaltiques permettent de définir trois grandes provinces magmatiques, séparées par les zones de fracture Malville (ZFM) et Gallieni. A l'est de la ZFM (60°45'E), les verres ont des compositions géochimiques qui
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Kirman, Sarah. "Cycles biogéochimiques et biodiversité en forêt tropicale humide : étude d'une succession primaire sur coulées basaltiques (La Réunion, Océan Indien)." Aix-Marseille 3, 2003. http://www.theses.fr/2003AIX30002.

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Le but de ce travail est de déterminer le rôle de la biodiversité dans les cycles biogéochimiques en milieu forestier tropical humide sur une chronoséquence de coulées basaltiques de 0 à 500 ans (La Réunion, Océan Indien). Dans la forêt mature des variations inter et intra annuelles des retombées de litière et des flux d'éléments sont notées. Les retombées de litière et les flux d'éléments montrent une relation positive avec la température avec un pic de production en période cyclonique. La biodiversité et la biomasse augmentent avec l'âge des coulées. La composition spécifique est dominée, su
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Bézos, Antoine. "Etude des éléments lithophiles et fortement sidérophiles (Pd, Pt, Ru et Ir) dans les basaltes des dorsales océaniques." Paris 7, 2003. http://www.theses.fr/2003PA077014.

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Jones, William Burrell. "Geochemistry and petrogenesis of basalts from Broken Ridge and Naturaliste Plateau, SE Indian Ocean." Thesis, Massachusetts Institute of Technology, 1991. http://hdl.handle.net/1721.1/54348.

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Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1991.<br>Includes bibliographical references (leaves 39-41).<br>by William Burrell Jones.<br>M.S.
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Humler, Eric. "Etude petrologique des basaltes oceaniques (ocean indien, mer rouge ocean atlantique) et continentaux (trapps du deccan, inde) : fonctionnement des reservoirs magmatiques." Université Louis Pasteur (Strasbourg) (1971-2008), 1989. http://www.theses.fr/1989STR13252.

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Ce travail a eu pour objet de rechercher des indices petrologiques permettant de mettre en evidence la presence de reservoirs magmatiques, de quantifier leur duree d'activite, de definir leur fonctionnement dynamique et d'etudier leur influence sur la geochimie des laves. Cette etude a porte sur les basaltes des trois dorsales oceaniques de l'ocean indien, de la dorsale medio-atlantique, de la mer rouge a 18n et, en domaine continental, des trapps du deccan entre nagpur et bombay. L'etude petrologique des basaltes permet de dire s'il y a melange ou non. C'est une condition necessaire mais non
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NAFZIGER, JEAN-MICHEL. "Petrologie et geochimie des basaltes de la dorsale centrale-indienne a 2150's (ocean indien) : segmentation a petite echelle des reservoirs magmatiques et du manteau." Université Louis Pasteur (Strasbourg) (1971-2008), 1995. http://www.theses.fr/1995STR13051.

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Sur la dorsale centrale-indienne, dorsale de type intermediaire (5,2 cm/an), 24 sites ont ete dragues dans une zone de 70 par 80 km a 2150's afin de determiner le comportement et la segmentation a petite echelle des reservoirs magmatiques et du manteau. Cette portion de dorsale est limitee au se par une zone de fracture et constituee de 3 unites le long de l'axe: 2 segments en forme de sablier se propageant l'un vers l'autre depuis 0,72 ma et qui sont separes par une discontinuite de troisieme ordre a 2145's. Les echantillons recoltes sont des basaltes a plagioclase et olivine peu ou pas alter
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Diop, Habib Elhadji Sy. "Geochemical investigation of basalts from Trois Menestrels, Kerguelen Archipelago." Thesis, Manhattan, Kan. : Kansas State University, 2008. http://hdl.handle.net/2097/947.

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Ricci, Jaime. "Investigating environmental response to Afro-Arabian flood basalt volcanism with elemental analysis of oligocene carbonate sediments from Odp Leg 115 site 709, Indian Ocean." Thesis, University of Iowa, 2012. https://ir.uiowa.edu/etd/3374.

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The goal of this project is to investigate potential environmental responses to the extensive volcanism associated with the Afro-Arabian Large Igneous Province, by analyzing major and trace element contents in the carbonate phase of Oligocene sediments from Ocean Drilling Program Leg 115 Site 709. These sediments were deposited above the carbonate compensation depth and span the main eruption interval of the Afro-Arabian Province at ~30 Ma based on the presence of correlated volcanic ash layers. Large Igneous Provinces erupt large magma volumes (>0.1 million km3) over a short time period (<1 m
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Catry, Thibault. "Magma injections and destabilization of basaltic volcanoes : A numerical study : Application to La Reunion (Indian ocean, France) and Stromboli (Tyrrhenian sea, Italy)." Phd thesis, Université de la Réunion, 2011. http://tel.archives-ouvertes.fr/tel-00805509.

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Most basaltic volcanoes are affected by recurrent lateral instabilities during their evolution. Numerous factors have been shown to be involved in the process of flank destabilization occurring over long periods of time or by instantaneous failures. However, the role of these factors on the mechanical behaviour and stability of volcanic edifices is poorly-constrained as lateral failure usually results from the combined effects of several parameters. Our study focuses on the morphological and structural comparison of two end-member basaltic systems, La Reunion (Indian ocean, France) and Strombo
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Catry, Thibault <1985&gt. "Magma injections and destabilization of basaltic volcanoes: a numerical study. Application to La Reunion (Indian ocean, France) and Stromboli (Tyrrhenian sea, Italy)." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2011. http://amsdottorato.unibo.it/3904/.

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Most basaltic volcanoes are affected by recurrent lateral instabilities during their evolution. Numerous factors have been shown to be involved in the process of flank destabilization occurring over long periods of time or by instantaneous failures. However, the role of these factors on the mechanical behaviour and stability of volcanic edifices is poorly-constrained as lateral failure usually results from the combined effects of several parameters. Our study focuses on the morphological and structural comparison of two end-member basaltic systems, La Reunion (Indian ocean, France) and Strombo
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Books on the topic "Basalte – Indien, Océan"

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Sylvander, Brendan A. The Southeast Indian Ridge water contents of MORB glasses and chemical effects of propagating rifts. 1998.

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Book chapters on the topic "Basalte – Indien, Océan"

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Natland, James. "Indian ocean crust." In Oceanic Basalts. Springer US, 1991. http://dx.doi.org/10.1007/978-1-4615-3540-9_12.

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Natland, James. "Indian ocean crust." In Oceanic Basalts. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3042-4_12.

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Join, Jean-Lambert, Jean-Luc Folio, Anli Bourhane, and Jean-Christophe Comte. "Groundwater Resources on Active Basaltic Volcanoes: Conceptual Models from La Réunion Island and Grande Comore." In Active Volcanoes of the Southwest Indian Ocean. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-31395-0_5.

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Sato, Hiroshi, Kentaro Nakamura, Hidenori Kumagai, et al. "Petrology and Geochemistry of Mid-Ocean Ridge Basalts from the Southern Central Indian Ridge." In Subseafloor Biosphere Linked to Hydrothermal Systems. Springer Japan, 2014. http://dx.doi.org/10.1007/978-4-431-54865-2_13.

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Das, Souvik, and Asish R. Basu. "Origin of the Indus ophiolite linked to the mantle transition zone (410–660 km)." In Plate Tectonics, Ophiolites, and Societal Significance of Geology: A Celebration of the Career of Eldridge Moores. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2552(02).

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ABSTRACT The southeast Ladakh (India) area displays one of the best-preserved ophiolite sections in this planet, in places up to 10 km thick, along the southern bank of the Indus River. Recently, in situ, ultrahigh-pressure (UHP) mineralogical evidence from the mantle transition zone (MTZ; ∼410–660 km) with diamond and reduced fluids were discovered from two peridotite bodies in the basal mantle part of this Indus ophiolite. Ultrahigh-pressure phases were also found by early workers from podiform chromitites of another coeval Neo-Tethyan ophiolite in southern Tibet. However, the MTZ phases in the Indus ophiolite are found in silicate peridotites, but not in metallic chromitites, and the peridotitic UHP phases show systematic and contiguous phase transitions from the MTZ to shallower depth, unlike the discrete UHP inclusions, all in Tibetan chromitites. We observe consistent change in oxygen fugacity (fO2) and fluid composition from (C-H + H2) to (CO2 + H2O) in the upwelling peridotitic mantle, causing melting to produce mid-ocean-ridge basalt (MORB). At shallow depths (&amp;lt;100 km) the free water stabilizes into hydrous phases, such as pargasitic amphibole, capable of storing water and preventing melting. Our discoveries provide unique insights into deep sub-oceanic-mantle processes, and link deep-mantle upwelling and MORB genesis. Moreover, the tectonic setting of Neo-Tethyan ophiolites has been a difficult problem since the birth of the plate-tectonics concept. This problem for the origin of ophiolites in mid-ocean-ridge versus supra-subduction zone settings clearly confused the findings from Indus ophiolites. However, in this contribution, we provide arguments in favor of mid-ocean-ridge origin for Indus ophiolite. In addition, we venture to revisit the “historical contingency” model of E.M. Moores and others for Neo-Tethyan ophiolite genesis based on the available evidence and have found that our new results strongly support the “historical contingency” model.
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Tatsumi, Y., and S. Nohda. "Geochemical Stratification in the Upper Mantle: Evidence from Leg 115 Basalts in the Indian Ocean." In Proceedings of the Ocean Drilling Program, 115 Scientific Results. Ocean Drilling Program, 1990. http://dx.doi.org/10.2973/odp.proc.sr.115.136.1990.

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Tatsumi, Y., and S. Nohda. "Geochemical Stratification in the Upper Mantle: Evidence from Leg 115 Basalts in the Indian Ocean." In Proceedings of the Ocean Drilling Program, 115 Scientific Results. Ocean Drilling Program, 1990. http://dx.doi.org/10.2973/odp.proc.sr.115.136.1991.

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Tamaki, K., K. Yamamoto, T. Furuta, and H. Yamamoto. "An Experiment of In-Situ Stress Estimation on Basaltic Rock Core Samples from Hole 758A, Ninetyeast Ridge, Indian Ocean." In Proceedings of the Ocean Drilling Program, 121 Scientific Results. Ocean Drilling Program, 1991. http://dx.doi.org/10.2973/odp.proc.sr.121.159.1991.

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Hutchison, Charles S. "The Geological Framework." In The Physical Geography of Southeast Asia. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199248025.003.0011.

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This chapter outlines the principal geological features of the region, extending from Myanmar and Taiwan in the north, southwards to include all the ASEAN countries, and extending as far as northern Australia. The present-day lithospheric plates and plate margins are described, and the Cenozoic evolution of the region discussed. Within a general framework of convergent plate tectonics, Southeast Asia is also characterized by important extensional tectonics, resulting in the world’s greatest concentration of deep-water marginal basins and Cenozoic sedimentary basins, which have become the focus of the petroleum industry. The pre-Cenozoic geology is too complex for an adequate analysis in this chapter and the reader is referred to Hutchison (1989) for further details. A chronological account summarizing the major geological changes in Southeast Asia is given in Figure 1.2. The main geographical features of the region were established in the Triassic, when the large lithospheric plate of Sinoburmalaya (also known as Sibumasu), which had earlier rifted from the Australian part of Gondwanaland, and collided with and became sutured onto South China and Indochina, together named Cathaysia. The result was a great mountain-building event known as the Indosinian orogeny. Major granites were emplaced during this orogeny, with which the tin and tungsten mineral deposits were genetically related. The orogeny resulted in general uplift and the formation of major new landmasses, which have predominantly persisted as the present-day regional physical geography of Southeast Asia. The Indo-Australian Plate is converging at an average rate of 70 mm a−1 in a 003° direction, pushed from the active South Indian Ocean spreading axis. For the most part it is composed of the Indian Ocean, formed of oceanic sea-floor basalt overlain by deep water. It forms a convergent plate margin with the continental Eurasian Plate, beneath which it subducts at the Sunda or Java Trench. The Eurasian continental plate protrudes as a peninsular extension (Sundaland) southwards as far as Singapore, continuing beneath the shallow Straits of Malacca and the Sunda Shelf as the island of Sumatra and the northwestern part of Borneo.
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Gibson, I. L., and A. D. Saunders. "Interpretation of Submarine Sequences of Pillowed and Massive Basaltic Units as Exemplified by Relations at Site 758, Ninetyeast Ridge, Indian Ocean." In Proceedings of the Ocean Drilling Program, 121 Scientific Results. Ocean Drilling Program, 1991. http://dx.doi.org/10.2973/odp.proc.sr.121.167.1991.

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Conference papers on the topic "Basalte – Indien, Océan"

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Reddy, R. Dileepkumar, Sridhar D. Iyer, S. Balakrishnan, and Rajneesh Bhutani. "Seawater Alteration of Central Indian Ocean Ridge Basalts: Geochemical and Isotopic Evidences." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2179.

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