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Relevant bibliographies by topics / Back-arc basins

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Academic literature on the topic 'Back-arc basins'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 January 2023

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Journal articles on the topic "Back-arc basins"

1

Martinez, Fernando, Kyoko Okino, Yasuhiko Ohara, Anna-Louise Reysenbach, and Shana Goffredi. "Back-Arc Basins." Oceanography 20, no. 1 (March 1, 2007): 116–27. http://dx.doi.org/10.5670/oceanog.2007.85.

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Kalra, Rajesh, Roberto Fainstein, and Srinivas Chandrashekar. "Unexplored deepwater basins of North Andaman Sea." Leading Edge 39, no. 8 (August 2020): 551–57. http://dx.doi.org/10.1190/tle39080551.1.

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Deepwater basins of the North Andaman Sea in the northern edge of the Far East Archipelago were assessed recently by state-of-the-art seismic technology. The North Andaman Sea embraces several Tertiary basins consisting of a forearc basin, a volcanic arc, and a back-arc basin. Their massive but largely unknown stratigraphy consists of deeper Neogene lacustrine and deltaic sediments that infill basal synrift half-grabens, blanketed by massive sequences of the Late Oligocene, Miocene, and recent strata. In the extensional forearc, the deeper seismic marker horizons were structurally mapped and identified by acoustic impedance contrasts as carbonates, mass-transport complexes, synrift, and basement. The shallower Pliocene and Pleistocene sequences are dominated by low-seismic-velocity hemipelagic clays that were investigated using seismic attributes and seismic inversion. In the back arc, the relatively larger graben features were affected by tectonic inversion contemporaneous with the foundering of the basin into deep water in the Late Miocene. In the forearc and back arc, main hydrocarbon plays are the rimmed Early Miocene carbonate platforms, the paralic and deltaic sediments beneath the platform, and the deepwater clastics of hemipelagic clays and sands that form the dominant strata of the Mio-Pliocene. This modern seismic exploration involved acquisition, processing, and interpretation to assess the hydrocarbon prospectivity of undrilled deepwater regions in the forearc and back arc.

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Magni, Valentina, John Naliboff, Manel Prada, and Carmen Gaina. "Ridge Jumps and Mantle Exhumation in Back-Arc Basins." Geosciences 11, no. 11 (November 19, 2021): 475. http://dx.doi.org/10.3390/geosciences11110475.

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Back-arc basins in continental settings can develop into oceanic basins, when extension lasts long enough to break up the continental lithosphere and allow mantle melting that generates new oceanic crust. Often, the basement of these basins is not only composed of oceanic crust, but also of exhumed mantle, fragments of continental crust, intrusive magmatic bodies, and a complex mid-ocean ridge system characterised by distinct relocations of the spreading centre. To better understand the dynamics that lead to these characteristic structures in back-arc basins, we performed 2D numerical models of continental extension with asymmetric and time-dependent boundary conditions that simulate episodic trench retreat. We find that, in all models, episodic extension leads to rift and/or ridge jumps. In our parameter space, the length of the jump ranges between 1 and 65 km and the timing necessary to produce a new spreading ridge varies between 0.4 and 7 Myr. With the shortest duration of the first extensional phase, we observe a strong asymmetry in the margins of the basin, with the margin further from trench being characterised by outcropping lithospheric mantle and a long section of thinned continental crust. In other cases, ridge jump creates two consecutive oceanic basins, leaving a continental fragment and exhumed mantle in between the two basins. Finally, when the first extensional phase is long enough to form a well-developed oceanic basin (>35 km long), we observe a very short intra-oceanic ridge jump. Our models are able to reproduce many of the structures observed in back-arc basins today, showing that the transient nature of trench retreat that leads to episodes of fast and slow extension is the cause of ridge jumps, mantle exhumation, and continental fragments formation.

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Stern, Robert J., Ping-Nan Lin, Julie D. Morris, Michael C. Jackson, Patricia Fryer, Sherman H. Bloomer, and Emi Ito. "Enriched back-arc basin basalts from the northern Mariana Trough: implications for the magmatic evolution of back-arc basins." Earth and Planetary Science Letters 100, no. 1-3 (October 1990): 210–25. http://dx.doi.org/10.1016/0012-821x(90)90186-2.

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Loreto, Maria Filomena, Camilla Palmiotto, Filippo Muccini, Valentina Ferrante, and Nevio Zitellini. "Inverted Basins by Africa–Eurasia Convergence at the Southern Back-Arc Tyrrhenian Basin." Geosciences 11, no. 3 (March 4, 2021): 117. http://dx.doi.org/10.3390/geosciences11030117.

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The southern part of Tyrrhenian back-arc basin (NW Sicily), formed due to the rifting and spreading processes in back-arc setting, is currently undergoing contractional tectonics. The analysis of seismic reflection profiles integrated with bathymetry, magnetic data and seismicity allowed us to map a widespread contractional tectonics structures, such as positive flower structures, anticlines and inverted normal faults, which deform the sedimentary sequence of the intra-slope basins. Two main tectonic phases have been recognised: (i) a Pliocene extensional phase, active during the opening of the Vavilov Basin, which was responsible for the formation of elongated basins bounded by faulted continental blocks and controlled by the tear of subducting lithosphere; (ii) a contractional phase related to the Africa-Eurasia convergence coeval with the opening of the Marsili Basin during the Quaternary time. The lithospheric tear occurred along the Drepano paleo-STEP (Subduction-Transform-Edge-Propagator) fault, where the upwelling of mantle, intruding the continental crust, formed a ridge. Since Pliocene, most of the contractional deformation has been focused along this ridge, becoming a good candidate for a future subduction initiation zone.

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Langmuir, C., A. Bezos, S. Escrig, and S. Parman. "Hydrous mantle melting at ridges and back-arc basins." Geochimica et Cosmochimica Acta 70, no. 18 (August 2006): A341. http://dx.doi.org/10.1016/j.gca.2006.06.691.

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Romagny, Adrien, Laurent Jolivet, Armel Menant, Eloïse Bessière, Agnès Maillard, Albane Canva, Christian Gorini, and Romain Augier. "Detailed tectonic reconstructions of the Western Mediterranean region for the last 35 Ma, insights on driving mechanisms." BSGF - Earth Sciences Bulletin 191 (2020): 37. http://dx.doi.org/10.1051/bsgf/2020040.

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Slab retreat, slab tearing and interactions of slabs are first-order drivers of the deformation of the overriding lithosphere. An independent description of the tectonic evolution of the back-arc and peripheral regions is a pre-requisite to test the proposed conceptual, analogue and numerical models of these complex dynamics in 3-D. We propose here a new series of detailed kinematics and tectonic reconstructions from 35 Ma to the Present shedding light on the driving mechanisms of back-arc rifting in the Mediterranean where several back-arc basins all started to form in the Oligocene. The step-by-step backward reconstructions lead to an initial situation 35 Ma ago with two subduction zones with opposite direction, below the AlKaPeCa block (i.e. belonging to the Alboran, Kabylies, Peloritani, Calabrian internal zones). Extension directions are quite variable and extension rates in these basins are high compared to the Africa-Eurasia convergence velocity. The highest rates are found in the Western Mediterranean, the Liguro-Provençal, Alboran and Tyrrhenian basins. These reconstructions are based on shortening rates in the peripheral mountain belts, extension rates in the basins, paleomagnetic rotations, pressure-temperature-time paths of metamorphic complexes within the internal zones of orogens, and kinematics of the large bounding plates. Results allow visualizing the interactions between the Alps, Apennines, Pyrenean-Cantabrian belt, Betic Cordillera and Rif, as well as back-arc basins. These back-arc basins formed at the emplacement of mountain belts with superimposed volcanic arcs, thus with thick, hot and weak crusts explaining the formation of metamorphic core complexes and the exhumation of large portions of lower crustal domains during rifting. They emphasize the role of transfer faults zones accommodating differential rates of retreat above slab tears and their relations with magmatism. Several transfer zones are identified, separating four different kinematic domains, the largest one being the Catalan-Balearic-Sicily Transfer Zone. Their integration in the wider Mediterranean realm and a comparison of motion paths calculated in several kinematic frameworks with mantle fabric shows that fast slab retreat was the main driver of back-arc extension in this region and that large-scale convection was a subsidiary driver for the pre-8 Ma period, though it became dominant afterward. Slab retreat and back-arc extension was mostly NW-SE until ∼ 20 Ma and the docking of the AlKaPeCa continental blocks along the northern margin of Africa induced a slab detachment that propagated eastward and westward, thus inducing a change in the direction of extension from NW-SE to E-W. Fast slab retreat between 32 and 8 Ma and induced asthenospheric flow have prevented the transmission of the horizontal compression due to Africa-Eurasia convergence from Africa to Eurasia and favored instead upper-plate extension driven by slab retreat. Once slab retreat had slowed down in the Late Miocene, this N-S compression was felt and recorded again from the High Atlas to the Paris Basin.

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Loreto, Maria Filomena. "Editorial of Special Issue “Tectonics and Morphology of Back-Arc Basins”." Geosciences 12, no. 2 (February 14, 2022): 86. http://dx.doi.org/10.3390/geosciences12020086.

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Di Giulio, Andrea, Chiara Amadori, Pierre Mueller, and Antonio Langone. "Role of the Down-Bending Plate as a Detrital Source in Convergent Systems Revealed by U–Pb Dating of Zircon Grains: Insights from the Southern Andes and Western Italian Alps." Minerals 10, no. 7 (July 16, 2020): 632. http://dx.doi.org/10.3390/min10070632.

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In convergent zones, several parts of the geodynamic system (e.g., continental margins, back-arc regions) can be deformed, uplifted, and eroded through time, each of them potentially delivering clastic sediments to neighboring basins. Tectonically driven events are mostly recorded in syntectonic clastic systems accumulated into different kinds of basins: trench, fore-arc, and back-arc basins in subduction zones and foredeep, thrust-top, and episutural basins in collisional settings. The most widely used tools for provenance analysis of synorogenic sediments and for unraveling the tectonic evolution of convergent zones are sandstone petrography and U–Pb dating of detrital zircon. In this paper, we present a comparison of previously published data discussing how these techniques are used to constrain provenance reconstructions and contribute to a better understanding of the tectonic evolution of (i) the Cretaceous transition from extensional to compressional regimes in the back-arc region of the southern Andean system; and (ii) the involvement of the passive European continental margin in the Western Alps subduction system during impending Alpine collision. In both cases, sediments delivered from the down-bending continental block are significantly involved. Our findings highlight its role as a detrital source, which is generally underestimated or even ignored in current tectonic models.

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Aplonov, Sergei, Kenneth J. Hsu, and Vitali Ustritsky. "Relict back-arc basins of Eurasia and their hydrocarbon potentials." Island Arc 1, no. 1 (August 1992): 71–77. http://dx.doi.org/10.1111/j.1440-1738.1992.tb00059.x.

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Dissertations / Theses on the topic "Back-arc basins"

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Schellart, Wouter Pieter. "Subduction rollback, arc formation and back-arc extension." Monash University, School of Geosciences, 2003. http://arrow.monash.edu.au/hdl/1959.1/9485.

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Anderson, Melissa. "Relationships Between Tectonics, Volcanism, and Hydrothermal Venting in the New Hebrides and Mariana Back-Arc Basins, Western Pacific." Thesis, Université d'Ottawa / University of Ottawa, 2018. http://hdl.handle.net/10393/37341.

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Understanding the controls on the distribution and type of hydrothermal venting in modern oceanic spreading environments is key to developing tools for exploration and understanding the metallogeny of ancient massive sulfide deposits. Compared to mid-ocean ridges, subduction zones are characterized by additional tectonic complexities, including arc-ridge collisions, arc rotations, pre-existing structures, and variable distances to the arc. This thesis addresses the question, “How do tectonic complexities associated with subduction influence the structure and volcanic evolution of a back-arc basin, and how do they affect the distribution and type of hydrothermal venting?” A multi-scaled approach was used to address this question in the nascent back-arc region of the New Hebrides and in the more advanced stages of opening of the Mariana back-arc basin. In the New Hebrides, an arc-ridge collision segmented the volcanic front and affected the southern and northern back-arc regions in different ways. In the southern Coriolis Troughs (CT), voluminous eruptions are closely linked to the ridge collision, forming a large shield volcano in the near-arc region (Nifonea Volcano). The caldera-hosted eruptions produced high-temperature but short-lived magmatic-hydrothermal activity restricted to the shield volcano. In the northern Jean Charcot Troughs (JCT), ridge collision caused a reversal in the rotation of the arc, reducing extension in the south and increasing extension in the north. Unlike the CT, extension in the JCT is strongly affected by pre-existing structures, which form irregular widely-spaced grabens and volcanic ridges and magmatism in the central part of the back-arc. Here, hydrothermal venting is focused along deeply penetrating faults, associated with widespread tectonic extension. Detailed studies of the mineralogy and geochemistry of the ore and alteration at the Tinakula deposit reveal that massive sulfide accumulation in the region dominated by tectonic extension is characterized by longer-lived, lower-temperature venting than at Nifonea. Hydrothermal activity in the JCT at Tinakula is dominated by (1) long-lived heat from an underlying magma source; (2) fluid circulation along a fissure with long-lived or reactivated permeability; (3) enrichment in fluid-mobile elements such as Ba that are transported at low temperature; (4) mixing of cold seawater with hydrothermal fluids within the permeable volcaniclastic substrate and at the seafloor; (5) water depth controls on maximum hydrothermal vent temperatures; and (6) reduced permeability of the host volcaniclastic succession at the site of mineralization caused by precipitation of alteration minerals and sulfates, focusing fluid flow. The different styles of volcanic and hydrothermal activity closely resemble those of mid-ocean ridge environments in areas that are dominated by tectonic rather than magmatic extension. A comparison with the more advanced stages of rifting and segmentation of the Mariana back-arc demonstrates that Mid-Ocean Ridge (MOR)-type structural and magmatic controls on hydrothermal activity are important during all stages of back-arc basin evolution. This work highlights the diversity of volcanic eruption styles and hydrothermal venting from the earliest stages of back-arc rifting to the advanced stages of basin opening and shows that processes normally associated with MOR-type spreading are directly analogous to back-arc basin systems. However, additional tectonic complexities (e.g., ridge-arc collisions) have a major impact on the location and type of magmatic and hydrothermal activity at back-arc spreading centers, with important implications for understanding ancient volcanic-hosted massive sulfide deposits that mainly formed in back-arc basins.

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Witte, Jan [Verfasser]. "Multi-scale and uncertainty assessment of contractional thick-skinned structures in petroleum basins of the Andean back-arc / Jan Witte." Berlin : Freie Universität Berlin, 2020. http://d-nb.info/1223925692/34.

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4

Satsukawa, Takako. "Interactions magma-roche, déformation à haute température et anisotropie sismique dans le manteau de la transition continent-océan et dans la lithosphère océanique." Thesis, Montpellier 2, 2012. http://www.theses.fr/2012MON20014/document.

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Cette thèse regroupe deux études distinctes, qui documentent le contrôle des microstructures sur les propriétés sismiques des roches. La première partie traite du développement des orientations préférentielles cristallographiques (OPC) dans le manteau supérieur, associé aux interactions liquide/magma-roche, enregistré dans des xénolites de péridotites du bassin d'arrière-arc de la mer du Japon. Les caractéristiques microstucturales et géochimiques des échantillons étudiés montrent que l'ouverture arrière-arc active est associée à une déformation du manteau supérieure similaire à celle observée dans l'ophiolite d'Oman. L'initiation de l'extension d'arrière-arc n'est pas associée à de fortes interactions entre percolation magmatique et déformation, en comparaison avec les zones de rifting continentales, probablement en raison des taille et durée relativement petites de l'épisode d'ouverture. La seconde partie présente une base de données unique d'OPC de plagioclase de roches mafiques plus ou moins déformées. Les OPC sont classées en 3 types principaux; leurs caractéristiques en fonction du régime de déformation (magmatique ou plastique) sont présentées et discutées. Les propriétés sismiques calculées des roches gabbroiques montrent que l'anisotropie tend à croitre avec l'intensité des fabriques, bien qu'elle soit généralement faible, en raison des effets opposés des olivines/clinopyroxènes et du plagioclase
This thesis compiles two distinct studies that both document the control of microstructures on rock seismic properties. The first part deals with the development of crystallographic preferred orientations (CPO) in the uppermost mantle associated with melt/fluid-rock interactions, recorded in peridotites xenoliths from the Japan sea back-arc basin. The microstructural and geochemical characteristics of the studied samples reveal that active spreading is associated to uppermost mantle deformation similar to that observed in the Oman ophiolite. At the onset of back-arc spreading, there are no strong interactions between melt percolation and deformation in comparison to continental rift zones, probably due to the relatively small size and short duration of the spreading event. The second part presents a unique database of plagioclase CPO from variously deformed mafic rocks. CPO are grouped in three main types; their characteristics as a function of deformation regime (magmatic or crystal-plastic) are outlined and discussed. Calculated seismic properties of gabbroic rocks show that anisotropy tends to increase as a function of fabric strength, although it is generally weak, due to the competing effect of olivine/clinopyroxene and plagioclase

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Blake, Elizabeth Anne. "Community Structure and Biogeography of Mussel Bed Communities at Pacific Hydrothermal Vents: Lau and North Fiji Back-Arc Basins, 32° S---East Pacific Rise, and 38° S---Pacific Antarctic Ridge." W&M ScholarWorks, 2006. https://scholarworks.wm.edu/etd/1539626850.

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Rosenbaum, Gideon. "Tectonic reconstruction of the Alpine orogen in the western Mediterranean region." Monash University, School of Geosciences, 2003. http://arrow.monash.edu.au/hdl/1959.1/9481.

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Desmet, Alain. "Ophiolites et séries basaltiques crétacées des régions caraïbes et nordandines : bassins marginaux, dorsales ou plateaux océaniques ?" Nancy 1, 1994. http://www.theses.fr/1994NAN10313.

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Les régions caraïbes et nordandines comportent, au crétacé, des séries magmatiques basiques, volcaniques ou ophiolitiques. L'étude petrologique analytique (majeurs, traces, terres rares, microsonde) de quelques séries du Costa Rica, de Colombie et d'Équateur, a permis leur identification magmatique et dynamique. La comparaison des laves à certaines séries volcaniques océaniques actuelles a conduit à une réinterprétation magmatique et géodynamique globale. Au Costa Rica, la péninsule de Santa Elena est formée d'une large nappe ophiolitique tholeiitique avec péridotites, cumulats gabbroiques et dolerites diverses (n-morb). Les iles Murcielago sont couvertes de ferrobasaltes t-morb. Santa Elena représente un témoin de croute océanique crétacée mis en place vers 70 ma et Murcielago un lambeau de plateau océanique soudé à l'Amérique centrale. La Colombie offre, au crétacé, et du nord au sud de la cordillère occidentale, un large éventail de formations océaniques: la série du Boqueron de Toyo, à volcanisme basaltique et intrusions diorito-tonalitiques (92 ma) témoigne du fonctionnement d'un arc insulaire immature. La série d'Altamira, a cumulats gabbroiques et basaltes primitifs illustre l'ouverture vers 80 ma d'un bassin en arrière de l'arc précédent. Le massif de Bolivar, correspond, avec ses cumulats tholeiitiques (i ou iia), a la croute océanique. La coupe de Buenaventura a Buga, avec ses nappes empilées riches en sédiments océaniques et en basaltes de type t-morb évoque des terrains constitués en plateau océanique et accrétés à la marge sud-américaine. En Équateur, le crétacé supérieur de la cordillère occidentale offre une situation analogue: des lambeaux de croute océanique sont dispersés le long d'une grande suture ophiolitique oblitérée par l'arc volcanique de Macuchi. La série de la Quebrada San Juan est l'équivalent de celle de Bolivar. Les basaltes (t-morb) du Grupo Pinon de la cote correspondent aussi à du matériel de plateau océanique accrété au bâti sud-américain

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O'Leary, Julie Ann Asimow Paul David. "Hydrogen isotope geochemistry of the mantle : constraints from back arc basin basalts and mantle xenoliths /." Diss., Pasadena, Calif. : California Institute of Technology, 2007. http://resolver.caltech.edu/CaltechETD:etd-12182006-072449.

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Shaw, Alison M. "Noble gas and major volatile systematics of the Manus Back-Arc basin and the Central American Arc : tracing source mixing, contamination and degassing /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 2003. http://wwwlib.umi.com/cr/ucsd/fullcit?p3091338.

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Fugate, Earl L. "NONLINEAR SYSTEM MODELING UTILIZING NEURAL NETWORKS: AN APPLICATION TO THE DOUBLE SIDED ARC WELDING PROCESS." Lexington, Ky. : [University of Kentucky Libraries], 2005. http://lib.uky.edu/ETD/ukyelen2005t00307/etd.pdf.

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Thesis (M.S.)--University of Kentucky, 2005.
Title from document title page (viewed on November 8, 2005). Document formatted into pages; contains vi, 64 p. : ill. Includes abstract and vita. Includes bibliographical references (p. 61-63).

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Books on the topic "Back-arc basins"

1

Kagami, Hiroo. Isotopic evidence for primitive mantle beneath the Sea of Japan, a young back arc basin. Misasa, Japan: Institute for Study of the Earth's Interior, Okayama University, 1986.

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The Ordovician basin in the Puna of NW Argentina and N Chile: Geodynamic evolution from back-arc to foreland basin. Stuttgart: Schweizerbart, 1990.

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H. de la R. Winter. A cratonic-foreland model for Witwatersrand Basin-Development in a continental, back-arc, plate-tectonic setting. Johannesburg: University of the Witwatersrand, 1986.

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Chin, Carol Sue. Hydrothermal activity along the northern Mid-Atlantic Ridge and in the Bransfield Strait backarc basin, Antarctica. 1998.

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1953-, Taylor Brian, ed. Backarc basins: Tectonics and magmatism. New York: Plenum Press, 1995.

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III, Pitman Walter C., and Manik Talwani. Island Arcs Deep Sea Trenches and Back-Arc Basins. Wiley & Sons, Limited, John, 2013.

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Christie, David M., Sharon Givens, Sang-Mook Lee, and Charles R. Fisher. Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions. Wiley & Sons, Limited, John, 2013.

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(Editor), David M. Christie, Charles R. Fisher (Editor), Sang-Mook Lee (Editor), and Sharon Givens (Editor), eds. Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions (Geophysical Monograph). Amer Geophysical Union, 2006.

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Book chapters on the topic "Back-arc basins"

1

Wilson, Marjorie. "Back-arc basins." In Igneous Petrogenesis, 227–42. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-94-010-9388-0_8.

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Saunders, Andrew, and John Tarney. "Back-arc basins." In Oceanic Basalts, 219–63. Boston, MA: Springer US, 1991. http://dx.doi.org/10.1007/978-1-4615-3540-9_10.

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Saunders, Andrew, and John Tarney. "Back-arc basins." In Oceanic Basalts, 219–63. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3042-4_10.

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Martinez, Fernando, and Brian Taylor. "Modes of crustal accretion in back-arc basins: Inferences from the Lau Basin." In Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions, 5–30. Washington, D. C.: American Geophysical Union, 2006. http://dx.doi.org/10.1029/166gm03.

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Takai, Ken, Satoshi Nakagawa, Anna-Louise Reysenbach, and Joost Hoek. "Microbial ecology of mid-ocean ridges and back-arc basins." In Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions, 185–213. Washington, D. C.: American Geophysical Union, 2006. http://dx.doi.org/10.1029/166gm10.

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Langmuir, C. H., A. Bézos, S. Escrig, and S. W. Parman. "Chemical systematics and hydrous melting of the mantle in back-arc basins." In Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions, 87–146. Washington, D. C.: American Geophysical Union, 2006. http://dx.doi.org/10.1029/166gm07.

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Desbruyères, Daniel, Jun Hashimoto, and Marie-Claire Fabri. "Composition and biogeography of hydrothermal vent communities in Western Pacific Back-Arc Basins." In Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions, 215–34. Washington, D. C.: American Geophysical Union, 2006. http://dx.doi.org/10.1029/166gm11.

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Kobayashi, Kazuo. "Non-Isostatic Slab-Support for Island Arcs and Back-Arc Basins." In International Association of Geodesy Symposia, 297–304. Berlin, Heidelberg: Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-662-03482-8_41.

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Shemenda, Alexander I. "Jumps of Subduction Zones, Subduction Reversal, and Closing of Back Arc Basins." In Subduction, 134–73. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-0952-9_5.

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Wiens, Douglas A., Nobukazu Seama, and James A. Conder. "Mantle structure and flow patterns beneath active back-arc basins inferred from passive seismic and electromagnetic methods." In Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions, 43–62. Washington, D. C.: American Geophysical Union, 2006. http://dx.doi.org/10.1029/166gm05.

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Conference papers on the topic "Back-arc basins"

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Vasey, Dylan, Eric Cowgill, and Kari M. Cooper. "GEOCHEMISTRY OF MODERN CONTINENTAL BACK-ARC BASINS AND TRIASSIC-JURASSIC COLLISION-INDUCED BACK-ARC SPREADING IN THE CAUCASUS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-360020.

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Schäfer, Wiebke, Manuel Keith, Marcel Regelous, Francois Holtz, and Reiner Klemd. "Trace elements in magmatic sulphide droplets from island arcs, back-arc basins and mid-ocean ridges." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12894.

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3

Goo Choi, B. "A NE-SW Trend Wrench Fault System and Hydrocarbon Exploration in the Back-Arc Basins, Offshore Korea." In 59th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.131.gen1997_d021.

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"The Relationship of Organic Components to Source Rocks Types Based on Biomarker Data at Central Sumatra Basin." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-sg-168.

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A biomarker study is used to observe the quality level of a hydrocarbon compound deposited on the source rock. The presence of Botryococcus braunii algae, Pediastrum algae, and other lacustrine algae is thought to be a contributing factor to petroleum in lacustrine basins throughout Southeast Asia. Botryococcus braunii is a group of green algae and belongs to the Trebouxiophyceae class. The purpose of this study is to discuss the relationship between organic compounds and the type of source rock in the Central Sumatra Basin. The Central Sumatra Basin is a back-arc basin that develops along the edge of the Sunda shelf in Southeast Asia. This basin was formed by the moving of the submergence of the Indian Ocean plate relative to the North and infiltrates the Asian Continent plate. The data used in this study is taken from several literatures/references in biomarker analysis where qualitative analysis was carried out, such as: matching the readings of compounds contained in the chromatogram and associate them with classification in some existing literatures where the selection of organic components that had an effect on geological analysis was carried out. An explanation of some of the data obtained along with the chromatogram and geological analysis and interpretation can be seen in this paper. Some conclusions can be drawn from this research in the form of qualitative analysis of organic components to define the maturity of the hydrocarbon and suspect the source organic materials of the hydrocarbon in source rocks. The explanation of the main biomarkers that must be considered when analyzing oil or source rock samples is to know the characteristic of the hydrocarbon and correlate it with reaction during the deposition.

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Permana, Aziz, Mateos Naiola, Daniel Siregar, Syaiful Damuar, Pambudi Suseno, Sakti Parsaulian, Dirsya Siki, and Ilham Barustan. "Low Resistivity Reservoir Identification of Gumai Formation Using Weighted Scoring Method in West Benakat, South Sumatra Basin, Indonesia." In SPE Annual Technical Conference and Exhibition. SPE, 2022. http://dx.doi.org/10.2118/210109-ms.

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Abstract The mature oil field of West Benakat is located in the South Sumatra Basin, one of the most hydrocarbon prolific Indonesian tertiary back-arc basins in Indonesia. Since its discovery in 1933, West Benakat Field has been operating and producing oil for nearly nine decades from Talang Akar Formation (TAF) as the main sand reservoir target with good porosity and permeability. Recently, Talang Akar reservoirs have been depleted through massive development programs, whereas more than 290 wells have been drilled for exploration, production, and injection wells. Decreasing oil production pushes the company's need for an alternative method that can increase oil production through subsurface evaluation in West Benakat Field to find the upside potential besides Talang Akar. One of the best alternative ways focused on the low resistivity pay zone from Gumai Formation (GUF) and Air Benakat Formation (ABF). The qualitative analysis through several well log data in Gumai Formation confirms the potential of low resistivity shaly sand reservoirs, GUF-1, GUF-2, and GUF-3, with neutron-density crossover. However, Talang Akar sand has an average resistivity value equally above 10 ohms. The low resistivity reservoir in Gumai turbidite deep marine sand could be occurred because of high shale content, fine grain sand, and the presence of laminated conductive clay minerals, such as glauconite. However, a low resistivity reservoir was initially considered unattractive because many major reservoirs which contain hydrocarbon would have a high resistivity value. Generally, the conventional petrophysical approach for low resistivity reservoirs in Gumai or Air Benakat Sand could lead to bias and pessimistic interpretation, yet in some cases, rocks with low resistivity have the potential to become hydrocarbon reservoirs. This study discusses how to identify and evaluate low resistivity pay zones and the success story of proving the Gumai hydrocarbon potential in West Benakat Field, South Sumatra.

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Esestime, P., H. Kearns, and P. J. Hargreaves. "The Balearic Basin in the West-Mediterranean - A Back-arc Basin or a Foreland-foredeep Basin?" In 77th EAGE Conference and Exhibition 2015. Netherlands: EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201412668.

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Kargl, S., P. Y. Chenet, B. Yoo, and H. G. Im. "Petroleum System Analysis for a Back-Arc Basin Offshore South Korea - The Ulleung Basin." In 68th EAGE Conference and Exhibition incorporating SPE EUROPEC 2006. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609.201402246.

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LoBianco, Samuel J. C., Eben B. Hodgin, and Francis A. Macdonald. "WESTWARD JURASSIC BACK-ARC BASIN MIGRATION IN THE CENTRAL ANDEAN CORDILLERA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-323406.

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Gorojovsky, Lauren, Olivier Alard, and Simon Turner. "Sulfur, Selenium, Tellurium, and Copper Systematics in the Manus Back-Arc Basin." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.865.

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Wyld, Sandra J., and James E. Wright. "JURASSIC BACK-ARC IGNEOUS PROVINCE OF THE NORTHERN GREAT BASIN: EVIDENCE FOR SLAB BREAK-OFF FOLLOWING ARC COLLISION." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-340652.

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Reports on the topic "Back-arc basins"

1

Johnston, D. The Noggin Cove Formation, Carmanville map area, northeast Newfoundland: a back-arc basin volcanic complex. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/133579.

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2

Manor, M. J., and S. J. Piercey. Whole-rock lithogeochemistry, Nd-Hf isotopes, and in situ zircon geochemistry of VMS-related felsic rocks, Finlayson Lake VMS district, Yukon. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328992.

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The Finlayson Lake district in southeastern Yukon is composed of a Late Paleozoic arc-backarc system that consists of metamorphosed volcanic, plutonic, and sedimentary rocks of the Yukon-Tanana and Slide Mountain terranes. These rocks host &gt;40 Mt of polymetallic resources in numerous occurrences and styles of volcanogenic massive sulphide (VMS) mineralization. Geochemical and isotopic data from these rocks support previous interpretations that volcanism and plutonism occurred in arc-marginal arc (e.g., Fire Lake formation) and continental back-arc basin environments (e.g., Kudz Ze Kayah formation, Wind Lake formation, and Wolverine Lake group) where felsic magmatism formed from varying mixtures of crust- and mantle-derived material. The rocks have elevated high field strength element (HFSE) and rare earth element (REE) concentrations, and evolved to chondritic isotopic signatures, in VMS-proximal stratigraphy relative to VMS-barren assemblages. These geochemical features reflect the petrogenetic conditions that generated felsic rocks and likely played a role in the localization of VMS mineralization in the district. Preliminary in situ zircon chemistry supports these arguments with Th/U and Hf isotopic fingerprinting, where it is interpreted that the VMS-bearing lithofacies formed via crustal melting and mixing with increased juvenile, mafic magmatism; rocks that were less prospective have predominantly crustal signatures. These observations are consistent with the formation of VMS-related felsic rocks by basaltic underplating, crustal melting, and basalt-crustal melt mixing within an extensional setting. This work offers a unique perspective on magmatic petrogenesis that underscores the importance of integrating whole-rock with mineral-scale geochemistry in the characterization of VMS-related stratigraphy.

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Kellett, D. A., N. Rogers, C. R. van Staal, and R. A. Wilson. Timing of progressive salinic orogeny D1/D2 deformation by in situ 40Ar/39Ar dating of cleavage domains within Tetagouche-Exploits back-arc basin, New Brunswick. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297628.

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