Relevant bibliographies by topics / IODP 355

Academic literature on the topic 'IODP 355'

Author: Grafiati
Published: 10 December 2022
Last updated: 29 January 2023

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Journal articles on the topic "IODP 355"

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Hahn, A., M. G. Bowen, P. D. Clift, D. K. Kulhanek, and M. W. Lyle. "Testing the analytical performance of handheld XRF using marine sediments of IODP Expedition 355." Geological Magazine 157, no. 6 (April 4, 2019): 956–60. http://dx.doi.org/10.1017/s0016756819000189.

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AbstractObtaining geochemical profiles using X-ray fluorescent (XRF) techniques has become a standard procedure in many sediment core studies. The resulting datasets are not only important tools for palaeoclimatic and palaeoceanographic reconstructions, but also for stratigraphic correlation. The International Ocean Discovery Program (IODP) has therefore recently introduced shipboard application of a handheld XRF device, making geochemical data directly available to the science party. In all XRF scanning techniques, the physical properties of wet core halves cause substantial analytical deviations. In order to obtain estimates of element concentrations (e.g. for quantitative analyses of fluxes or mass-balance calculations), a calibration of the scanning data is required. We test whether results from the handheld XRF analysis on discrete samples are suitable for calibrating scanning data. Log-ratios with Ca as a common denominator were calculated. The comparison between the handheld device and conventional measurements show that the latter provide high-quality data describing Al, Si, K, Ca, Ti, Mn, Fe, Zn, Rb and Sr content (R2 compared with conventional measurements: ln(Al/Ca) = 0.99, ln(Si/Ca) = 0.98, ln(K/Ca) = 0.99, ln(Ti/Ca) = 0.99, ln(Mn/Ca) = 0.99, ln(Fe/Ca) = 0.99, ln(Zn/Ca) = 0.99 and ln(Sr/Ca) = 0.99). Our results imply that discrete measurements using the shipboard handheld analyser are suitable for the calibration of XRF scanning data. Our test was performed on downcore sediments from IODP Expedition 355 that display a wide variety of lithologies of both terrestrial and marine origin. The implication is that our findings are valid on a general scale and that shipboard handheld XRF analysis on discrete samples should be used for calibrating XRF scanning data.
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Garzanti, Eduardo, Sergio Andò, and Giovanni Vezzoli. "Provenance of Cenozoic Indus Fan Sediments (IODP Sites U1456 and U1457)." Journal of Sedimentary Research 90, no. 9 (September 1, 2020): 1114–27. http://dx.doi.org/10.2110/jsr.2019-195.

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ABSTRACT Provenance analysis of IODP Expedition 355 cores in the Laxmi Basin sheds new light on the erosional evolution of the Himalayan belt and its western syntaxis during the Neogene and on large-scale mass-wasting and magmatic events that affected the western continental margin of India in the mid-Miocene and early Paleocene. In the cored Laxmi Basin succession, heavy minerals are far less affected by selective diagenetic dissolution than in foreland-basin sandstones exposed along the Himalayan front. Occurrence of euhedral aegirine and apatite in lower Paleocene mudrocks can be tied to alkaline volcanism affecting the adjacent western Indian margin during the late stage of Deccan activity. In the mid-Miocene Nataraja Slide (the second-largest mass-transport deposit reported from passive margins worldwide), dominant carbonate detritus and depleted heavy-mineral suites (including apatite, garnet, and locally augite or rare aegirine) reveal gravitational failure and sliding of the entire succession of carbonate and siliciclastic Paleogene to lower Neogene strata originally accumulated offshore of the Saurashtra margin of western India. Contrary to previous inferences, reworking of Indus-derived detritus by the slide was negligible. The overlying upper Miocene to lower Pleistocene turbidite package has the same feldspatho-litho-quartzose to litho-feldspatho-quartzose signature of modern Indus fluvio-deltaic sand, indicating that amphibolite-facies metamorphic rocks have been widely exposed in the Himalaya–Karakorum orogen since at least the mid-Miocene. Pleistocene nannofossil oozes with planktonic foraminifera at the top of the fan contain a very subordinate litho-feldspatho-quartzose terrigenous fraction including augitic clinopyroxene, suggesting mixing of dominant biogenic debris with minor detritus contributed both by the Indus River and by a river draining western peninsular India, possibly the paleo-Narmada or the paleo-Tapti.
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Andò, S., S. Aharonovich, A. Hahn, SC George, PD Clift, and E. Garzanti. "Integrating heavy-mineral, geochemical and biomarker analyses of Plio-Pleistocene sandy and silty turbidites: a novel approach for provenance studies (Indus Fan, IODP Expedition 355)." Geological Magazine 157, no. 6 (August 14, 2019): 929–38. http://dx.doi.org/10.1017/s0016756819000773.

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AbstractA multidisciplinary mineralogical, geochemical and biomarker study of Indus Fan sediments cored during International Ocean Discovery Program (IODP) Expedition 355 to the Laxmi Basin was carried out to define the different compositional signatures of sand, silt and clay. Upper Pliocene – lower Pleistocene turbidites from sites U1456 and U1457 were selected as the best candidates for this study. The integrated dataset presented here was obtained by coupling traditional and innovative bulk-sediment and single-mineral techniques on the same samples. Turbiditic deposits mostly consist of medium to fine silt, including rich and diverse heavy-mineral assemblages. Such a fine grain size forced us to push the limits of high-resolution quantitative heavy-mineral analysis down to as low as 5 μm. Heavy-mineral analysis allowed us to establish a Himalayan origin of the detritus in the studied turbidites. Heavy-mineral concentrations are higher in channel-fill than in overbank deposits. Mineralogical and geochemical data concur in revealing that fast-settling ultradense minerals such as zircon are preferentially concentrated in channel-fill deposits, whereas the top of overbank deposits are notably enriched with slow-settling platy phyllosilicates. Biomarker analysis represents a most suitable complementary technique that is able to investigate the provenance signature of the finer sediment fraction, largely consisting of clay. This technique allowed us to identify a largely terrigenous origin of organic matter at Site U1456 and an open marine origin at Site U1457. The latter site lies closer to the Laxmi Ridge, where thermal maturity increases with depth to reach the early oil window (127°C at c. 320 m below the seafloor).
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Chen, Hongjin, Zhaokai Xu, Peter D. Clift, Dhongil Lim, Boo-Keun Khim, and Zhaojie Yu. "Orbital-scale evolution of the Indian summer monsoon since 1.2 Ma: Evidence from clay mineral records at IODP Expedition 355 Site U1456 in the eastern Arabian Sea." Journal of Asian Earth Sciences 174 (May 2019): 11–22. http://dx.doi.org/10.1016/j.jseaes.2018.10.012.

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Khim, Boo-Keun, Jongmin Lee, Sanbeom Ha, Jingu Park, Dhananjai K. Pandey, Peter D. Clift, Denise K. Kulhanek, et al. "Variations in δ13C values of sedimentary organic matter since late Miocene time in the Indus Fan (IODP Site 1457) of the eastern Arabian Sea." Geological Magazine 157, no. 6 (January 7, 2019): 1012–21. http://dx.doi.org/10.1017/s0016756818000870.

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AbstractA 1108.6 m long core was recovered at Site U1457 located on the Indus Fan in the Laxmi Basin of the eastern Arabian Sea during IODP Expedition 355. Shipboard examinations defined five lithologic units (I to V) of the lower Paleocene to Holocene sedimentary sequence. In this study, δ13C values of sedimentary organic matter (SOM) confirm the differentiation of the lithologic units and further divide units III and IV into two subunits (1 and 2). Based on the underlying assumption that the SOM is decided primarily by a mixture of marine and terrestrial origins, δ13CSOM values at Site U1457 provide information on the terrestrial catchment conditions since late Miocene time. Low δ13CSOM values from late Miocene to late Pleistocene times are similar (c. −22.0 ‰) for the most part, reflecting a consistent contribution of terrestrial organic matter from the catchment areas characterized by dominant C3 land plants. Significantly lower δ13CSOM values (c. −24.0 ‰) in Unit III-2 (∼8 to ∼7 Ma) might be due to a greater input of C3 terrestrial organic matter. The increase in δ13CSOM values at ∼7 Ma and the appearance of high δ13CSOM values (c. −18.0 ‰) within Unit III-1 (∼7 to ∼2 Ma) indicate that C4 biomass overwhelmed the terrestrial catchment environment as a result of enhanced terrestrial aridity in the Himalayan foreland. The three-end-member simple mixing model, estimating the relative contributions of SOM from terrestrial C3 and C4 plants and marine phytoplankton, supports our interpretation of the distribution of C3 and C4 land plants in the terrestrial catchment environment.
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Pandey, D. K., Anju Pandey, Peter D. Clift, Nisha Nair, Prerna Ramesh, Denise K. Kulhanek, and Rajeev Yadav. "Flexural subsidence analysis of the Laxmi Basin, Arabian Sea and its tectonic implications." Geological Magazine 157, no. 6 (December 18, 2018): 834–47. http://dx.doi.org/10.1017/s0016756818000833.

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AbstractTwo-dimensional flexural backstripping and thermal modelling (assuming laterally variable stretching) is applied along regional depth-converted interpreted seismic profiles from the Laxmi Basin in the Arabian Sea. Results from reverse post-rift flexural modelling reveal considerable basin-wide subsidence in response to the crustal geodynamics during and after the last extensional phase. Unloading of the stratigraphy allows us to estimate the degree of laterally varying extension, assuming thermal subsidence and pure shear. High degrees of extension in the basin centre predict considerable water depths at the time of rift cessation, consistent with deep drilling data. We suggest that regional extension prior to Paleocene time could have fuelled variable subsidence in the Laxmi Basin but that extension is less than seen in typical oceanic lithosphere. Volcanic loading by the seamounts shortly after extension has flexed the basin and implies an effective elastic thickness (Te) at that time of ∼6 km. Reconstruction of the seamount top near sea level at the end of emplacement indicates no major transient uplift potentially linked to the Deccan mantle plume activity. Backstripping of post-rift sediments from interpreted seismic profiles supports the presence of a hyper-thinned crust underneath the Laxmi Basin, with β factors reaching >7 in the basin centre and ∼3 across much of the basin width. Computations of decompacted sediment accumulation rates in light of new results from IODP Expedition 355 show that basin sedimentation peaked during early–middle Miocene time, possibly coeval with uplift and erosion of the Himalayan–Tibetan Plateau driven by strong summer monsoon rains.
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Dailey, Sarah K., Peter D. Clift, Denise K. Kulhanek, Jerzy Blusztajn, Claire M. Routledge, Gérôme Calvès, Paul O’Sullivan, et al. "Large-scale mass wasting on the Miocene continental margin of western India." GSA Bulletin 132, no. 1-2 (May 9, 2019): 85–112. http://dx.doi.org/10.1130/b35158.1.

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Abstract A giant mass-transport complex was recently discovered in the eastern Arabian Sea, exceeding in volume all but one other known complex on passive margins worldwide. The complex, named the Nataraja Slide, was drilled by International Ocean Discovery Program (IODP) Expedition 355 in two locations where it is ∼300 m (Site U1456) and ∼200 m thick (Site U1457). The top of this mass-transport complex is defined by the presence of both reworked microfossil assemblages and deformation structures, such as folding and faulting. The deposit consists of two main phases of mass wasting, each consisting of smaller pulses, with generally fining-upward cycles, all emplaced just prior to 10.8 Ma based on biostratigraphy. The base of the deposit at each site is composed largely of matrix-supported carbonate breccia that is interpreted as the product of debris-flows. In the first phase, these breccias alternate with well-sorted calcarenites deposited from a high-energy current, coherent limestone blocks that are derived directly from the Indian continental margin, and a few clastic mudstone beds. In the second phase, at the top of the deposit, muddy turbidites dominate and become increasingly more siliciclastic. At Site U1456, where both phases are seen, a 20-m section of hemipelagic mudstone is present, overlain by a ∼40-m-thick section of calcarenite and slumped interbedded mud and siltstone. Bulk sediment geochemistry, heavy-mineral analysis, clay mineralogy, isotope geochemistry, and detrital zircon U-Pb ages constrain the provenance of the clastic, muddy material to being reworked, Indus-derived sediment, with input from western Indian rivers (e.g., Narmada and Tapti rivers), and some material from the Deccan Traps. The carbonate blocks found within the breccias are shallow-water limestones from the outer western Indian continental shelf, which was oversteepened from enhanced clastic sediment delivery during the mid-Miocene. The final emplacement of the material was likely related to seismicity as there are modern intraplate earthquakes close to the source of the slide. Although we hypothesize that this area is at low risk for future mass wasting events, it should be noted that other oversteepened continental margins around the world could be at risk for mass failure as large as the Nataraja Slide.
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Naeini, Emitis Natali, Hugo De Bruyn, Ewald M. Bronkhorst, and Jan D’haese. "Case Series on the Long-Term Effect of Three Different Types of Maxillary Implant-Supported Overdentures on Clinical Outcomes and Complications." Journal of Clinical Medicine 11, no. 8 (April 18, 2022): 2251. http://dx.doi.org/10.3390/jcm11082251.

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(1) Long-term data on maxillary implant overdentures (IODs) are scarce. This case series evaluated three types of IODs supported by six, four or three implants (Anyridge®, Mega’Gen Implant Co., Ltd., Daegu, South-Korea), after 3–5 years in function. (2) A total of 31 patients, with 132 implants, were non-randomly allocated based on available bone or financial limitations. IOD-6 received a telescopic overdenture; IOD-4 a bar; and IOD-3, non-connected implants with locator abutments. Implant survival, bone level changes, probing pocket depth (PPD), plaque index, bleeding on probing (BOP), and technical, biological and aesthetic complications were registered. Impact of suprastructures on bone loss and PPD was analyzed using mixed-effect linear regression models. Differences between groups were analyzed using the ANOVA test for BOP, and Kruskal Wallis test for complications. (3) In total, 23 patients participated in the follow-up (9 female, 14 male), with average age of 62.2 years; 7, 11 and 5 patients in IOD-6, IOD-4 and IOD-3, respectively. Implant survival after 4.4 years on average, was 98% in total; 100%, 97.8% and 93.3% for IOD-6, IOD-4 and IOD-3, respectively. Mean bone loss corresponded to 0.68 mm (SD 1.06, range −4.57–1.51), 0.39 mm (SD 1.06, range −3.6–2.43), and 1.42 mm (SD 1.68, range −5.11–0.74) for IOD-6, IOD-4 and IOD-3, respectively. A statistically significant difference was seen in bone level when comparing IOD-6 to IOD-3 (p = 0.044), and IOD-4 to IOD-3 (p = 0.018). Mean PPD was 3.8 mm (SD: 0.69; range 2.5–5.3), 3.5 mm (SD 0.59; range 2.33–5), and 3.2 mm (SD 0.56; range 2–4) for IOD-6, IOD-4 and IOD-3, respectively, and differed significantly between IOD-6 and IOD-3 (p = 0.029). Incidence of peri-implantitis was 1%. No differences were seen for complications between groups. (4) Maxillary IOD supported by four to six implants is the most reliable treatment regarding implant survival and peri-implant health. More research is needed in the clinical outcomes, in particular the peri-implant health, and complications of maxillary IODs, especially with a reduced number of implants.
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Teagle, D. A. H., B. Ildefonse, and P. Blum. "IODP Expedition 335: Deep Sampling in ODP Hole 1256D." Scientific Drilling 13 (April 1, 2012): 28–34. http://dx.doi.org/10.5194/sd-13-28-2012.

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Observations of the gabbroic layers of untectonized ocean crust are essential to test theoretical models of the accretion of new crust at mid-ocean ridges. Integrated Ocean Drilling Program (IODP) Expedition 335 ("Superfast Spreading Rate Crust 4") returned to Ocean Drilling Program (ODP) Hole 1256D with the intention of deepening this reference penetration of intact ocean crust a significant distance (~350 m) into cumulate gabbros. Three earlier cruises to Hole 1256D (ODP 206, IODP 309/312) have drilled through the sediments, lavas, and dikes and 100 m into a complex dike-gabbro transition zone. <br><br> Operations on IODP Expedition 335 proved challenging throughout, with almost three weeks spent re-opening and securing unstable sections of the hole. When coring commenced, the comprehensive destruction of the coring bit required further remedial operations to remove junk and huge volumes of accumulated drill cuttings. Hole-cleaning operations using junk baskets were successful, and they recovered large irregular samples that document a hitherto unseen sequence of evolving geological conditions and the intimate coupling between temporally and spatially intercalated intrusive, hydrothermal, contact-metamorphic, partial melting, and retrogressive processes. <br><br> Hole 1256D is now clean of junk, and it has been thoroughly cleared of the drill cuttings that hampered operations during this and previous expeditions. At the end of Expedition 335, we briefly resumed coring before undertaking cementing operations to secure problematic intervals. To ensure the greatest scientific return from the huge efforts to stabilize this primary ocean lithosphere reference site, it would be prudent to resume the deepening of Hole 1256D in the nearest possible future while it is open to full depth. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.13.04.2011" target="_blank">10.2204/iodp.sd.13.04.2011</a>
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Matsuzaki, Kenji M., Hiroshi Nishi, Hiroki Hayashi, Noritoshi Suzuki, Babu R. Gyawali, Minoru Ikehara, Takuyuki Tanaka, and Reishi Takashima. "Radiolarian biostratigraphic scheme and stable oxygen isotope stratigraphy in southern Japan (IODP Expedition 315 Site C0001)." Newsletters on Stratigraphy 47, no. 1 (April 1, 2014): 107–30. http://dx.doi.org/10.1127/0078-0421/2014/0044.

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Dissertations / Theses on the topic "IODP 355"

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Carter, Samantha Cassie. "Improving our understanding of the marine barium cycle and constructing a new archive of erosion and sediment transport." The Ohio State University, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=osu1593602009469204.

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Courtillat, Margot. "Reconstruction des changements océanographiques et atmosphériques dans l’Océan Indien Oriental (NO-Australie, IODP Exp 356) pendant le quaternaire." Thesis, Perpignan, 2019. http://www.theses.fr/2019PERP0029/document.

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Les sédiments marins des sites de forage U1460 et U1461 recueillis pendant l’expédition IODP 356 constituent l’un des rares enregistrements au niveau du plateau australien Nord-Ouest. Ils fournissent des informations sur l’intensité de l’aridité en Australie pendant les principaux cycles glaciaires-interglaciaires du Quaternaire, en raison de leur proximité avec le continent. Outre la reconstitution du climat continental, ces sériés sédimentaires permettent de reconstruire le fonctionnement des courants océaniques passés au large de la côte Ouest australienne.Sur le site U1461, la chronostratigraphie a permis d’identifier deux glaciations majeures du Pléistocène (MIS 2 et MIS 12). Les assemblages de la microfaune benthique (principalement les foraminifères benthiques, les coraux et les bryozoaires) ont été analysés afin de reconstruire les paléo-environnements et les paléo-profondeurs du milieu sédimentaire. Malgré la présence d’un hiatus dans l’enregistrement (incluant une partie du MIS 2 et l’ensemble du MIS 3-MIS 7), l’excellente conservation du contenu de la microfaune benthique suggère que les sédiments préservés peuvent être considérés comme in situ.Sur ce même site, les isotopes du Nd et du Sr ainsi que d’autres traceurs (à citer) déterminés dans les sédiments indiquent d’une part que les apports fluviaux ont probablement été réduits en raison de l'aridité accrue au cours du MIS 12, et d’autre part que la source des sédiments (principalement transportés par voie atmosphérique) pourrait se trouver au centre (Lake Eyre) ou à l’Est du continent (Murray-Darling Basin) australien. Le MIS 2 s’avère être l’une des périodes les plus sèches enregistrées en Australie avec des sources de poussière mixtes provenant de l’Est et de l’Ouest du continent. Des conditions plus humides pouvant correspondre au maximum de la Mousson d’été Indo-Australienne ont suivi après le maximum glaciaire.Sur le site U1460, une étude approfondie des assemblages de la méiofaune benthique et de l'abondance d’une espèce de foraminifère planctonique (Globorotalia mernardii ) donne de bons indices prouvant un changement majeur et soudain de la circulation océanique au cours de l'événement de Bruhnes Moyen (Mid-Bruhnes Event, MIS 11). L'une des hypothèses privilégiées pour ce changement pendant cette période serait liée à la mise en place du courant de Leeuwin moderne
IODP Expedition 356 Site U1461 and Site U1460 represents ones of the few records in the NW sector of the Australian shelf that provides information about aridity fluctuations in Australia during major glacial cycles of the Quaternary because of their proximity to the continent. At the same time, they are also providing information about former ocean currents around Australia.For the Site U1461 a combination of chronostratigraphic indicators revealed the (partial) preservation of two major glaciations (MIS 2 and MIS 12) in the sedimentary record. The faunal content (mainly benthic foraminifera, corals and bryozoans) was analyzed for estimating paleo-environments and depths in order to determine if these sediments have been remobilized by reworking processes. Despite the occurrence of a depositional hiatus (that includes part of the MIS 2 and the whole MIS 3-MIS 7 time interval), the excellent preservation of faunal content suggests that the preserved sediment can be considered in situ.The geochemical composition of the sediments (Nd and Sr radiogenic isotopes and major elements) measured in the U1461 indicates, riverine input was likely reduced because of enhanced aridity during the MIS 12, and the sediment provenance (mainly atmospheric dust) might come from the Central (Lake Eyre) or the eastern (Murray Darling Basin) parts of the continent. MIS 2 is confirmed to be one of the driest periods recorded in Australia with mixed dust sources from the eastern and western parts of the continent. More humid conditions followed the glacial maximum that might correspond to the peak of the Indian-Australian Summer Monsoon.For the Site U1460 a thorough study of the benthic meiofauna assemblages and of the abundance of G. mernardii give some strong evidences of a major and suddenly change in the oceanographic circulation during the Mid-Bruhnes –Event (MIS 11). One of the preferred hypothesis for this change is related to the set-up of the modern Leeuwin Current at this period
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Sanatan, Keir Aavon. "Characterizing the Evolution of Slab Inputs in the Earliest Stages of Subduction: Preliminary Evidence from the Fluid-Mobile Element (B, Cs, As, Li) Systematics of Izu-Bonin Boninitic Glasses Recovered During IODP Expedition 352." Scholar Commons, 2017. http://scholarcommons.usf.edu/etd/6755.

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Fluid-mobile elements (FMEs) such as B, Cs, As, Li and Tl can mobilize readily under low P-T conditions (0.2-0.5 GPa). This makes them effective geochemical tracers that can be used as a way of tracking fluid-rock exchanges at the shallow depths encountered in the earliest stages of subduction. The Izu-Bonin-Mariana (IBM) subduction system is unique in that it preserves a record of the sequences produced from the onset of subduction through the development of arc magmatism. International Ocean Discovery Program (IODP) Expedition 352 recovered >800m of boninite core material from the earliest IBM magmatic events. Select boninitic glasses from these IODP 352 cores, found mostly as selvages on the rinds of pillow lavas and as clasts within hyaloclastites, were examined via EPMA and laser ablation ICP-MS techniques. The boninite glasses analyzed were separated into two categories – low-silica boninite (LSB) and high-silica boninites (HSB), based on the bulk chemistry and mineralogy of the lithostratigraphic locations from which the glass samples occur in the drill core. LSB are the earlier erupted boninite series, which show both greater variation in extent of differentiation and reflect less depleted mantle sources than HSB. Boron concentrations in the Expedition 352 boninite glasses analyzed range from 0.08 to 12.91 ppm, arsenic contents vary from 0.15 to 3.26 ppm, and cesium varies from 0.01 to 0.91 ppm. Lithium concentrations in the boninites range from 1 to 18.35 ppm while Tl concentrations vary from 10 to 155 ppb. FME concentrations trend toward higher values in HSB than in LSB. Low-Si boninites appear to form via simple mixing of depleted mantle source and an FME enriched fluid endmember, which mobilizes B, As, Cs, (Tl) and Li very early in the subduction process. Coupled with inputs from upwelling mantle, this FME-rich fluid triggers fluid-fluxed boninite melting. The high-Si boninites reflect the addition of a subduction component with a higher Ba/La ratio than that of the depleted mantle; this higher ratio more closely resembles that of Mariana cherts from altered Pacific crust. Thus, the high-Si boninites are consistent with the fluid-fluxed melting of a highly depleted, harzburgitic mantle source and reflect inputs of two distinguishable slab-derived components, one that is sedimentary in nature and another that is FME-enriched. This model for melting that is more similar to the melting regime of modern arcs and reflects the transition from early extension-related melting into that of a “normal” subduction system.
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Bergmann, Fenna [Verfasser], Volkhard [Akademischer Betreuer] Spieß, Volkhard [Gutachter] Spieß, and Christian [Gutachter] Hübscher. "The Bengal Fan on different temporal and spatial scales : Integrating seismoacoustic and IODP Expedition 354 data to examine internal and external controls on depositional processes / Fenna Bergmann ; Gutachter: Volkhard Spieß, Christian Hübscher ; Betreuer: Volkhard Spieß." Bremen : Staats- und Universitätsbibliothek Bremen, 2018. http://d-nb.info/1175090131/34.

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Book chapters on the topic "IODP 355"

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Ganesh Kumar, A., R. Vijaya Raghavan, G. Dharani, and M. A. Atmanand. "Microbial Community Profile of Deep-Sea Sediment from Eastern Arabian Sea (IODP 355)." In Dynamics of the Earth System: Evolution, Processes and Interactions, 277–83. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40659-2_12.

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Kawsar, Masud, M. C. Manoj, Kohki Yoshida, Alan T. Baxter, and Brendan T. Reilly. "Morphological and Chemical Properties of Microtektite Grains from Bay of Bengal (IODP Expedition 354)." In Dynamics of the Earth System: Evolution, Processes and Interactions, 27–53. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40659-2_2.

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Das, Supriyo Kumar, Ujan Karmakar, Arunabha Dey, Sandip Agrahari, and Alf Ekblad. "Carbon Stable Isotope Source Signature of Bulk Organic Matter in Middle Bengal Fan Sediment Collected During IODP Expedition 354." In Dynamics of the Earth System: Evolution, Processes and Interactions, 91–99. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40659-2_5.

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Reynolds, S. J., C. F. Smith, C. J. Jones, J. A. McCleverty, D. C. Brower, and J. L. Templeton. "Dicarbonylnitrosyl{Tris(3,5-Dimethylpyrazolyl)Hydroborato}- Molybdenum(III) and Iodo-, Alkoxy-, and Alkylamido-Molybdenum(III) Derivatives." In Inorganic Syntheses, 4–9. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2007. http://dx.doi.org/10.1002/9780470132548.ch2.

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Lyle, M., and R. Saraswat. "Data report: revised Pleistocene sediment splice for Site U1457, IODP Expedition 355." In Proceedings of the International Ocean Discovery Program. International Ocean Discovery Program, 2019. http://dx.doi.org/10.14379/iodp.proc.355.202.2019.

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Carter, S. C., E. M. Griffith, and H. D. Scher. "Data report: 87Sr/86Sr in pore fluids from IODP Expedition 355 Arabian Sea Monsoon." In Proceedings of the International Ocean Discovery Program. International Ocean Discovery Program, 2017. http://dx.doi.org/10.14379/iodp.proc.355.201.2017.

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France-Lanord, C., V. Spiess, A. Klaus, R. R. Adhikari, S. K. Adhikari, J. J. Bahk, A. T. Baxter, et al. "Expedition 354 summary." In Proceedings of the International Ocean Discovery Program. International Ocean Discovery Program, 2016. http://dx.doi.org/10.14379/iodp/proc.354.101.2016.

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France-Lanord, C., V. Spiess, A. Klaus, R. R. Adhikari, S. K. Adhikari, J. J. Bahk, A. T. Baxter, et al. "Expedition 354 methods." In Proceedings of the International Ocean Discovery Program. International Ocean Discovery Program, 2016. http://dx.doi.org/10.14379/iodp/proc.354.102.2016.

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Gillis, K. M., J. E. Snow, A. Klaus, G. Guerin, N. Abe, N. Akizawa, G. Ceuleneer, et al. "Expedition 345 summary." In Proceedings of the IODP. Integrated Ocean Drilling Program, 2014. http://dx.doi.org/10.2204/iodp.proc.345.101.2014.

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Ashi, J., S. Lallemant, and H. Masago. "Expedition 315 summary." In Proceedings of the IODP. Integrated Ocean Drilling Program, 2009. http://dx.doi.org/10.2204/iodp.proc.314315316.121.2009.

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Conference papers on the topic "IODP 355"

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Zhou, Peng, Peter D. Clift, Jerzy S. Blusztajn, Dhananjai K. Pandey, and Daniel F. Stockli. "CLIMATE-TECTONIC INTERACTIONS RECORDED IN THE ARABIAN SEA: RESULTS FROM IODP EXPEDITION 355." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289544.

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Muniz, Ana Luiza, R. Oliveira, I. Peixoto, and Daniel Franco. "Análise cicloestratigráfica preliminar do sítio U1463C – Expedição 356 (IODP)." In International Congress of the Brazilian Geophysical Society&Expogef. Brazilian Geophysical Society, 2019. http://dx.doi.org/10.22564/16cisbgf2019.041.

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Shervais, John, Emily A. Haugen, Jeffrey Ryan, Marguerite Godard, Julie Prytulak, Kenji Shimizu, Timothy Chapman, et al. "CHEMOSTRATIGRAPHY OF SUBDUCTION INITIATION: IODP EXPEDITION 352 BONINITE AND FAB." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283837.

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Hill, Stephen, Jesse Scholpp, Jeffrey Ryan, and Antonio Luna. "COMPLEX MINERAL TEXTURES AND CHEMISTRIES IN BONINITES FROM IODP EXPEDITION 352." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314198.

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Haugen, Emily A., and John W. Shervais. "GEOCHEMICAL MODELING OF BONINITE AND FAB FROM IODP EXPEDITION 352, IZU-BONIN FOREARC." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285718.

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Tachambalath, Aswin Pradeep, Christian France-Lanord, Albert Galy, Thomas Rigaudier, and Julien Charreau. "Silicate weathering budget of Himalaya from IODP expedition 354 in the Bengal Fan." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.11903.

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Scholpp, Jesse, Stephen Hill, Antonio Luna, and Jeffrey Ryan. "EVIDENCE FOR HIGH PRESSURE AND TEMPERATURE CRYSTALLIZATION IN BONINITE SAMPLES RECOVERED DURING IODP EXPEDITION 352." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314170.

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Scholpp, Jesse, Bradford Mack, Antonio Luna, and Jeffrey Ryan. "MINERAL CHEMISTRY EVIDENCE FOR MAGMA MIXING IN BONINITES, SITES U1439 AND U1442, IODP EXPEDITION 352." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-290606.

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Galy, Albert. "Triple Oxygen and Hydrogen Isotopic Variations of Pore Waters from the Middle Bengal Fran (IODP Exp. 354)." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.780.

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Stern, Robert J., Mark K. Reagan, and Julian A. Pearce. "STUDYING AN OPHIOLITE IN ITS NATURAL ENVIRONMENT: IODP LEG 352 DRILLING IN THE IZU-BONIN-MARIANA FOREARC." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282752.

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