Gotowe bibliografie tematyczne / Ocean ridge basalts

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Gotowa bibliografia na temat „Ocean ridge basalts”

Autor: Grafiati

Data publikacji: 3 czerwca 2025

Data aktualizacji: 31 lipca 2025

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Artykuły w czasopismach na temat "Ocean ridge basalts"

Arvin, Mohsen, and Paul T. Robinson. "The petrogenesis and tectonic setting of lavas from the Baft Ophiolitic Mélange, southwest of Kerman, Iran." Canadian Journal of Earth Sciences 31, no. 5 (1994): 824–34. http://dx.doi.org/10.1139/e94-076.

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A Late Cretaceous ophiolite complex in the Baft area, southwest of Kerman, Iran, is characteristic of the Central Iranian Ophiolitic Mélange Belt, which wraps around the Lut Block. Despite the extensive tectonic disruption of the Baft complex, most ophiolitic lithologies are present and many original igneous contacts are preserved. A lack of cumulate gabbros within the sequence suggests that a large and continuous magma chamber did not exist beneath the Baft spreading axis. Geochemical data confirm the presence of two distinct compositional groups in the mafic lavas: (1) tholeiitic basalt and

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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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Sun, Kai, Tao Wu, Xuesong Liu, Xue-Gang Chen, and Chun-Feng Li. "Lithogeochemistry of the Mid-Ocean Ridge Basalts near the Fossil Ridge of the Southwest Sub-Basin, South China Sea." Minerals 10, no. 5 (2020): 465. http://dx.doi.org/10.3390/min10050465.

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Mid-ocean ridge basalts (MORB) in the South China Sea (SCS) record deep crust-mantle processes during seafloor spreading. We conducted a petrological and geochemical study on the MORBs obtained from the southwest sub-basin of the SCS at site U1433 and U1434 of the International Ocean Discovery Program (IODP) Expedition 349. Results show that MORBs at IODP site U1433 and U1434 are unaffected by seawater alteration, and all U1433 and the bulk of U1434 rocks belong to the sub-alkaline low-potassium tholeiitic basalt series. Samples collected from site U1433 and U1434 are enriched mid-ocean ridge

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Hu, Wen-Jun, Hong Zhong, Wei-Guang Zhu, and Zhong-Jie Bai. "Rift- and subduction-related crustal sequences in the Jinshajiang ophiolitic mélange, SW China: Insights into the eastern Paleo-Tethys." Lithosphere 11, no. 6 (2019): 821–33. http://dx.doi.org/10.1130/l1091.1.

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Abstract The Paleozoic Jinshajiang ophiolitic mélange in southwest China marks an important branch ocean (i.e., the Jinshajiang Ocean) of the Paleo-Tethys. Basic-intermediate rocks are widespread features in the mélange; their formation age is well known, but the petrogenesis has not been well studied, which means that the evolutionary history of the Jinshajiang Ocean is not well constrained. To understand the nature of the mélange and the ocean, we present a set of elemental and isotopic data from two typical crustal sequences in two areas of the Jinshajiang ophiolitic mélange, Zhiyong and Ba

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Andrew, Anne, and Colin I. Godwin. "Lead- and strontium-isotope geochemistry of the Karmutsen Formation, Vancouver Island, British Columbia." Canadian Journal of Earth Sciences 26, no. 5 (1989): 908–19. http://dx.doi.org/10.1139/e89-073.

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Lead-isotope whole-rock ratios of the Triassic flood basalts of the Karmutsen Formation are heterogeneous, with 206Pb/2MPb = 18.72–21.51, 207Pb/204Pb = 15.56–15.77, and 208Pb/204Pb = 38.16–40.15. Whole-rock lead initial ratios are coincident with galena analyses having 206Pb/204Pb = 18.1–19.0, 207Pb/204Pb = 15.53–15.60, and 208Pb/204Pb = 38.2–38.6. Lead, uranium, and thorium concentrations are greater than for mid-ocean-ridge basalts, less than for island arcs, but similar to those in ocean-island and continental flood basalts. Isotopic similarities exist between the Columbia River – Chilcotin

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HU, WEN-JUN, HONG ZHONG, WEI-GUANG ZHU, and XIAO-HU HE. "Elemental and Sr–Nd isotopic geochemistry of the basalts and microgabbros in the Shuanggou ophiolite, SW China: implication for the evolution of the Palaeotethys Ocean." Geological Magazine 152, no. 2 (2014): 210–24. http://dx.doi.org/10.1017/s0016756814000259.

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AbstractThe Early Palaeozoic Shuanggou ophiolite is the best-preserved part of the Ailaoshan ophiolite belt. The microgabbros (basaltic dykes) and basalts (basaltic lavas) show distinct characteristics in geochemistry, implying that their genetic mechanisms are different. With Al2O3 contents ranging from 14.7% to 17.0%, the microgabbros belong to low-alumina type. They exhibit normal mid-ocean-ridge basalt (N-MORB) -like trace elemental characteristics with positive εNd(t) values (9.7–11.6) and slightly variable (87Sr/86Sr)i ratios (0.7036–0.7046). In contrast, the basalts have high Al2O3 cont

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Li, Hengxu, Mengqi Gao, Xiaohui Ji, Zhaochong Zhang, Zhiguo Cheng, and M. Santosh. "Machine Learning-Based Tectonic Discrimination Using Basalt Element Geochemical Data: Insights into the Carboniferous–Permian Tectonic Regime of Western Tianshan Orogen." Minerals 15, no. 2 (2025): 122. https://doi.org/10.3390/min15020122.

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Identifying the tectonic setting of rocks is essential for gaining insights into the geological contexts in which these rocks were formed, aiding in tectonic plate reconstruction and enhancing our comprehensive understanding of the Earth’s history. The application of machine learning algorithms helps identify complex patterns and relationships between big data that may be overlooked by binary or ternary tectonomagmatic discrimination diagrams based on basalt compositions. In this study, three machine learning algorithms, i.e., Support Vector Machine (SVM), Random Forest (RF), and eXtreme Gradi

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Cousens, Brian, Jarda Dostal, and T. S. Hamilton. "A near-ridge origin for seamounts at the southern terminus of the Pratt-Welker Seamount Chain, northeast Pacific Ocean." Canadian Journal of Earth Sciences 36, no. 6 (1999): 1021–31. http://dx.doi.org/10.1139/e99-008.

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Three seamounts close to the south end of the Pratt-Welker Seamount Chain, Gulf of Alaska, have been sampled to test whether or not mantle plume-related volcanism extends south of Bowie Seamount. Lavas recovered from Oshawa, Drifters, and Graham seamounts are weathered, Mn-encrusted pillow lavas and sheet-flow fragments, commonly with glassy rims. The glasses and holocrystalline rocks are tholeiitic basalts, with light rare earth element depleted to flat primitive mantle normalized incompatible element patterns and radiogenic isotope compositions within the ranges of mid-ocean ridge and near-r

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Daspan, R.I, J.A Yakubu, and U.A. Lar. "GEOCHEMICAL CHARACTERISTICS OF GABBROIC INTRUSIVE BODIES IN THE SHA-KALERI YOUNGER GRANITE COMPLEX, CENTRAL NIGERIA." Continental J. Earth Sciences 2 (November 7, 2007): 7–13. https://doi.org/10.5281/zenodo.824281.

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Large discrete gabbroic intrusive bodies outcrop within the Tof sub-unit of the Sha-Kaleri Jurassic Younger Granite Complex, situated at the southwestern end of the Jos Plateau.They were sampled and analysed for their major and trace element compositions with a view to determining their geochemical characteristics and tectonic setting The gabbroic rocks co-exist with hybrid rocks of composition in-between the gabbros and the granite porphyry and the extrusive equivalent basaltic rocks. The rocks are composed essentially of plagioclase and hornblende with minor pyroxene (titaniferous augite) an

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Fujii, Toshitsugu. "Genesis of mid-ocean ridge basalts." Geological Society, London, Special Publications 42, no. 1 (1989): 137–46. http://dx.doi.org/10.1144/gsl.sp.1989.042.01.09.

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Rozprawy doktorskie na temat "Ocean ridge basalts"

Gale, Allison. "Perspectives on Ocean Ridge Basalts from the Segment to the Global Scale." Thesis, Harvard University, 2012. http://dissertations.umi.com/gsas.harvard:10560.

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This study addresses the influences on ridge basalt chemistry, through analysis of their major and trace element and isotopic composition at scales ranging from individual ridge segments to the entire length of the ridge system. Local-scale studies of basalts along the Mid-Atlantic Ridge shed light on crustal accretion at slow-spreading ridges, and on the nature of plume-ridge interaction in this region. We show that segments must have multiple supplies of magma delivered along their length, but with preferential delivery of magma to segment centers. Plume-ridge interaction near the Azores is

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Kinzler, Rosamond Joyce. "Experimental constraints on the generation and evolution of mid-ocean ridge basalts." Thesis, Massachusetts Institute of Technology, 1991. http://hdl.handle.net/1721.1/54342.

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Le, Roux Petrus Jacobus. "The geochemistry of selected mid-ocean ridge basalts from the Southern mid-Atlantic ridge (40°- 55°S)." Doctoral thesis, University of Cape Town, 2000. http://hdl.handle.net/11427/4207.

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Summary in English. Includes bibliographical references. In 1993, dredge-sampling from 40.6°S to 525.5°S, during cruise 9309 of the R/V Maurice Ewing, greatly increased the number of basalts recovered from this section of the southern Mid-Atlantic Ridge (SMAR), and significantly expanded the global suite of samples from slow-spreading ridges.

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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. Includes bibliographical references (leaves 39-41). by William Burrell Jones. M.S.

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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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Shea, Gregory Thomas Francis. "A petrologic study of basalts from the Magic Mountain hydorthermal area, Southern Explorer Ridge, northeast Pacific Ocean." Thesis, University of British Columbia, 1987. http://hdl.handle.net/2429/41970.

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The Magic Mountain Hydrothermal Area (MMA) is a 5 km portion of the Southern Explorer Ridge (SER) centered at 49°46' and 130°20'W. It is a region of active hydrothermal activity located near the culmination of an unusually high standing spreading centre. Seafloor photographs, conductivity-temperature surveys and acoustic images have been used to determine the nature and extent of axial volcanism and tectonism as well as the associated hydrothermal activity. Major element and trace element whole rock analyses were obtained by x-ray flourescence spectrometry (XRF) for 25 recently formed

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Cordery, Matthew Jean. "Mantle convection, melt migration and the generation of basalts at mid-ocean ridges." Thesis, Massachusetts Institute of Technology, 1991. http://hdl.handle.net/1721.1/52936.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, and Woods Hole Oceanographic Institute, 1991. Includes bibliographical references (leaves 183-190). by Matthew Jean Cordery. Ph.D.

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Elkins, Lynne J. "Basalt petrogenesis beneath slow- and ultraslow-spreading Arctic mid-ocean ridges." Thesis, Massachusetts Institute of Technology, 2009. http://hdl.handle.net/1721.1/55327.

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Thesis (Ph. D.)--Joint Program in Marine Geology and Geophysics (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2009. Includes bibliographical references. To explore the ability of melting mafic lithologies to produce alkaline ocean-island basalts (OIB), an experimental study was carried out measuring clinopyroxene (Cpx)melt and garnet (Gt)-melt partition coefficients during silica-poor garnet pyroxenite melting for a suite of trace elements, including U and Th, at 2.5GPa and 1420-1450°C. Partitio

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Peterman, Kenneth James. "Determination of Oxygen Fugacity using Olivine-Melt Equilibrium: Implications for the Redox States of Mid-Ocean Ridge Basalt and Ocean Island Basalt Mantle Source Regions." The Ohio State University, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=osu1502803559889083.

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VERHOEST, LENA. "Sciogliere un mantello terrestre eterogeneo sotto un estremo gradiente termico." Doctoral thesis, Università degli studi di Modena e Reggio Emilia, 2022. https://hdl.handle.net/11380/1292196.

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Questa tesi esplora l'eterogeneità litologica del mantello suboceanico sorgente dei basalti eruttati lungo la Dorsale Medio-Oceanica (MORB). Sebbene l'eterogeneità del mantello vari a scala chilometrica, la composizione dei basalti eruttati all'asse della dorsale è in genere relativamente costante. Questo apparente paradosso deriva dall’alto grado di fusione parziale del mantello che media il contributo delle diverse litologie della sorgente al fuso aggregato riducendo la variabilità primaria. Un modo per distinguere il contributo delle singole litologie consite nell’esplorare la variazione co

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Książki na temat "Ocean ridge basalts"

Cordery, Matthew Jean. Mantle convection, melt migration and the generation of basalts at mid-ocean ridges. WHOI, 1991.

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Geological Survey (U.S.), ed. Geochemistry and petrography of basalt dredged on cruise L5-83-HW from Necker Ridge, Horizon and S.P. Lee Guyot, Central Pacific Ocean. Dept. of the Interior, U.S. Geological Survey, 1987.

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Loock, Gabriele M. Character and distribution of the Indian Ocean mantle domain: A study of the mantle source compositions of Lau Basin volcanics (SW-Pacific) and Indian Ocean mid-ocean ridge basalts. 1992.

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Livermore, Roy. All at Sea. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198717867.003.0009.

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According to first-generation plate tectonics, sea-floor spreading was nice and simple. Plates were pulled apart at mid-ocean ridges, and weak mantle rocks rose to fill the gap and began to melt. The resulting basaltic magma ascended into the crust, where it ponded to form linear ‘infinite onion’ magma chambers beneath the mid-ocean tennis-ball seam. At frequent intervals, vertical sheets of magma rose from these chambers to the surface, where they erupted to form new ocean floor or solidified to form dykes, in the process acquiring a magnetization corresponding to the geomagnetic field at the

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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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Pyle, Douglas G. Geochemistry of mid-ocean ridge basalt within and surrounding the Australian-Antarctic discordance. 1993.

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Pyle, Douglas G. Geochemistry of mid-ocean ridge basalt within and surrounding the Australian-Antarctic discordance. 1993.

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Części książek na temat "Ocean ridge basalts"

Elthon, Don. "Experimental phase petrology of mid-ocean ridge basalts." In Oceanic Basalts. Springer US, 1991. http://dx.doi.org/10.1007/978-1-4615-3540-9_6.

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Elthon, Don. "Experimental phase petrology of mid-ocean ridge basalts." In Oceanic Basalts. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3042-4_6.

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Langmuir, Charles H. "Mid-Ocean Ridge Basalts (MORB)." In Encyclopedia of Earth Sciences Series. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-39193-9_252-1.

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Langmuir, Charles H. "Mid-Ocean Ridge Basalts (MORB)." In Encyclopedia of Earth Sciences Series. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-39312-4_252.

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Langmuir, Charles H., Emily M. Klein, and Terry Plank. "Petrological Systematics of Mid-Ocean Ridge Basalts: Constraints on Melt Generation Beneath Ocean Ridges." In Mantle Flow and Melt Generation at Mid-Ocean Ridges. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm071p0183.

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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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Lundstrom, Craig C. "5. Uranium-series Disequilibria in Mid-ocean Ridge Basalts: Observations and Models of Basalt Genesis." In Uranium-series Geochemistry, edited by Bernard Bourdon, Gideon M. Henderson, Craig C. Lundstrom, and Simon Turner. De Gruyter, 2003. http://dx.doi.org/10.1515/9781501509308-010.

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Graham, David W. "8. Noble Gas Isotope Geochemistry of Mid-Ocean Ridge and Ocean Island Basalts: Characterization of Mantle Source Reservoirs." In Noble Gases, edited by Donald P. Porcelli, Chris J. Ballentine, and Rainer Wieler. De Gruyter, 2002. http://dx.doi.org/10.1515/9781501509056-010.

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Grove, Timothy L., Rosamond J. Kinzler, and Wilfred B. Bryan. "Fractionation of Mid-Ocean Ridge Basalt (MORB)." In Mantle Flow and Melt Generation at Mid-Ocean Ridges. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm071p0281.

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Thy, P. "Phase equilibrium constraints on the evolution of transitional and mildly alkalic Fe-Ti basalts in the rift zones of Iceland." In Evolution of Mid Ocean Ridges. American Geophysical Union, 1989. http://dx.doi.org/10.1029/gm057p0039.

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Streszczenia konferencji na temat "Ocean ridge basalts"

Michael, Peter. "Assimilation of Halite by Mid-Ocean Ridge Basalts." In Goldschmidt2021. European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.8202.

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Gu, Jesse T., and Nick Dygert. "3HE/22NE VARIATIONS AMONG OCEAN ISLAND, MID-OCEAN RIDGE, AND BACKARC BASALTS." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289252.

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Yang, Alexandra Yang, Yue Cai, Charles Langmuir, Steven L. Goldstein, and Peter Michael. "The Subduction Influence on Ocean Ridge Basalts and its Significance." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2973.

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Zhang, Zhaofeng, Weidong Sun, Hongli Zhu, and Fang Liu. "The cerium stable isotopic composition of mid-ocean ridge basalts." In Goldschmidt 2024. Geochemical Society, 2024. https://doi.org/10.46427/gold2024.22833.

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Ramamurty, Prabala, Teeda Kumar, E. V. S. S. K. Babu, and Abhay Mudholkar. "Vesicles and Sulfide globules in mid-ocean ridge basalts (MORB): A comprehensive study from the Carlsberg Ridge basalt glasses." In Goldschmidt 2024. Geochemical Society, 2024. https://doi.org/10.46427/gold2024.22163.

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Elkins, Lynne, and Sarah Lambart. "Melt modeling of U-series disequilibria in mid-ocean ridge basalts." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10057.

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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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Yang, Alexandra Yang, Charles Langmuir, Yue Cai, Peter Michael, Steven Goldstein, and Zhongxing Chen. "A subduction influence on ocean ridge basalts outside the Pacific subduction shield." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10363.

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Duvernay, Thomas, Patrick Ball, Shihao Jiang, and D. Rhodri Davies. "Coupled Geodynamical-Geochemical Perspectives on the Generation and Composition of Mid-Ocean Ridge Basalts." In Goldschmidt 2024. Geochemical Society, 2024. https://doi.org/10.46427/gold2024.21236.

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Rodney, Joel, Morten Andersen, Bramley Murton, and Tim Elliott. "Origin of enriched mid-ocean ridge basalts: A perspective from uranium and molybdenum isotope ratios." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.18644.

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Raporty organizacyjne na temat "Ocean ridge basalts"

Mueller, C., S. J. Piercey, M. G. Babechuk, and D. Copeland. Stratigraphy and lithogeochemistry of rocks from the Nugget Pond Deposit area, Baie Verte Peninsula, Newfoundland. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328989.

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Stratigraphic and lithogeochemical data were collected from selected drill core from the Nugget Pond gold deposit in the Betts Cove area, Newfoundland. The stratigraphy consists of a lower unit of basaltic rocks that are massive to pillowed (Mount Misery Formation). This is overlain by sedimentary rocks of the Scrape Point Formation that consist of lower unit of turbiditic siltstone and hematitic cherts/iron formations (the Nugget Pond member); the unit locally has a volcaniclastic rich-unit at its base and grades upwards into finer grained volcaniclastic/turbiditic rocks. This is capped by ba

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Knowledge summary, A deep-sea experiment on carbon dioxide storage in oceanic crust. CDRmare, 2022. http://dx.doi.org/10.3289/cdrmare.20.

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On Iceland, water enriched with carbon dioxide has been injected into the upper ocean crust since 2014 – and successfully. The carbon dioxide mineralises within a short time and is firmly bound for millions of years. However, since ocean crust only rises above sea level in a few places on Earth, researchers are currently investigating the option of injecting carbon dioxide into ocean regions where huge areas of suitable basalt crust lie at medium to great water depths. One possible advantage: In the deep sea subsurface, the carbon dioxide would either be stable as a liquid or dissolve in the s

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A deep-sea experiment on carbon dioxide storage in oceanic crust. CDRmare, 2022. http://dx.doi.org/10.3289/cdrmare.21.

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On Iceland, water enriched with carbon dioxide has been injected into the upper ocean crust since 2014 – and successfully. The carbon dioxide mineralises within a short time and is firmly bound for millions of years. However, since ocean crust only rises above sea level in a few places on Earth, researchers currently investigate the option of injecting carbon dioxide into ocean regions where huge areas of suitable basalt crust lie at medium to great water depths. One possible advantage: In the deep sea subsurface, the carbon dioxide would either be stable as a liquid or dissolve in the seawate

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A deep-sea experiment on carbon dioxide storage in oceanic crust - Version 2. CDRMare, 2023. http://dx.doi.org/10.3289/cdrmare.21_v2.

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Factsheet: On Iceland, water enriched with carbon dioxide has been injected into the upper ocean crust since 2014 – and successfully. The carbon dioxide mineralises within a short time and is firmly bound for millions of years. However, since ocean crust only rises above sea level in a few places on Earth, researchers currently investigate the option of injecting carbon dioxide into ocean regions where huge areas of suitable basalt crust lie at medium to great water depths. One possible advantage: In the deep sea subsurface, the carbon dioxide would either be stable as a liquid or dissolve in

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