Relevant bibliographies by topics / IODP 313

Academic literature on the topic 'IODP 313'

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Published: 10 December 2022
Last updated: 29 January 2023

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Journal articles on the topic "IODP 313"

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Katz, M. E., J. V. Browning, K. G. Miller, D. H. Monteverde, G. S. Mountain, and R. H. Williams. "Paleobathymetry and sequence stratigraphic interpretations from benthic foraminifera: Insights on New Jersey shelf architecture, IODP Expedition 313." Geosphere 9, no. 6 (October 11, 2013): 1488–513. http://dx.doi.org/10.1130/ges00872.1.

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Breuker, Anja, Susanne Stadler, and Axel Schippers. "Microbial community analysis of deeply buried marine sediments of the New Jersey shallow shelf (IODP Expedition 313)." FEMS Microbiology Ecology 85, no. 3 (May 29, 2013): 578–92. http://dx.doi.org/10.1111/1574-6941.12146.

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Proust, Jean-Noël, Hugo Pouderoux, Hisao Ando, Stephen P. Hesselbo, David M. Hodgson, Johanna Lofi, Marina Rabineau, and Peter J. Sugarman. "Facies architecture of Miocene subaqueous clinothems of the New Jersey passive margin: Results from IODP-ICDP Expedition 313." Geosphere 14, no. 4 (June 14, 2018): 1564–91. http://dx.doi.org/10.1130/ges01545.1.

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Prader, Sabine, Ulrich Kotthoff, Francine M. G. McCarthy, Gerhard Schmiedl, Timme H. Donders, and David R. Greenwood. "Vegetation and climate development of the New Jersey hinterland during the late Middle Miocene (IODP Expedition 313 Site M0027)." Palaeogeography, Palaeoclimatology, Palaeoecology 485 (November 2017): 854–68. http://dx.doi.org/10.1016/j.palaeo.2017.07.028.

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Mountain, G., and J. N. Proust. "The New Jersey Margin Scientific Drilling Project (IODP Expedition 313): Untangling the Record of Global and Local Sea-Level Changes." Scientific Drilling 10 (September 1, 2010): 26–34. http://dx.doi.org/10.5194/sd-10-26-2010.

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Nilsson, A., Y. S. Lee, I. Snowball, and M. Hill. "Magnetostratigraphic importance of secondary chemical remanent magnetizations carried by greigite (Fe3S4) in Miocene sediments, New Jersey shelf (IODP Expedition 313)." Geosphere 9, no. 3 (April 4, 2013): 510–20. http://dx.doi.org/10.1130/ges00854.1.

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Kotthoff, U., D. R. Greenwood, F. M. G. McCarthy, K. Müller-Navarra, and S. P. Hesselbo. "Vegetation and climate development on the North American Atlantic Coastal Plain from 33 to 13 million years ago (IODP Expedition 313)." Climate of the Past Discussions 9, no. 6 (December 13, 2013): 6551–603. http://dx.doi.org/10.5194/cpd-9-6551-2013.

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Abstract. We have investigated the palynology of sediment cores from Sites M0027 and M0029 of IODP Expedition 313 on the New Jersey shallow shelf, east coast of North America, spanning an age range of 33 to 13 million years before present. Additionally, a pollen assemblage from the Pleistocene was examined. The palynological results were statistically analyzed and complemented with pollen-based quantitative climate reconstructions. Transport-related bias of the pollen assemblages was identified via analysis of the ratio of terrestrial to marine palynomorphs, and considered when interpreting palaeovegetation and palaeoclimate from the pollen data. Results indicate that from the early Oligocene to the middle Miocene, the hinterland vegetation of the New Jersey shelf was characterized by oak-hickory forests in the lowlands and conifer-dominated vegetation in the highlands. The Oligocene witnessed several expansions of conifer forest, probably related to cooling events. The pollen-based climate data imply an increase in annual temperatures from ~12 °C to more than 15 °C during the Oligocene. The Mi-1 cooling event at the onset of the Miocene is reflected by an expansion of conifers and an annual temperature decrease by almost 3 °C, from 15 °C to 12.5 °C around 23 million years before present. Particularly low annual temperatures are also recorded for an interval around ~20 million years before present, which probably reflects the Mi-1aa cooling event. Generally, the Miocene ecosystem and climate conditions were very similar to those of the Oligocene in the hinterland of the New Jersey shelf. Miocene grasslands, as known from other areas in the USA during that time period, are not evident for the hinterland of the New Jersey shelf. Surprisingly, the palaeovegetation data for the hinterland of the New Jersey shelf do not show extraordinary changes during the Mid-Miocene climatic optimum at ~15 million years before present, except for a minor increase in deciduous-evergreen mixed forest taxa and a decrease in swamp forest taxa. Pollen-based annual temperature reconstructions show average annual temperatures of ~14 °C during the Mid-Miocene climatic optimum. We conclude that vegetation and regional climate in the hinterland of the New Jersey shelf did not react as sensitively to Oligocene and Miocene climate changes as other regions in North America or Europe. An additional explanation for the relatively low regional temperatures reconstructed for the Mid-Miocene climatic optimum could be an uplift of the Appalachian Mountains during the Miocene. The Pleistocene pollen assemblage probably derives from the Marine Isotope Chron 7 or 5e and shows climate conditions similar to present-day.
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Pierre, Catherine, Marie-Madeleine Blanc-Valleron, Omar Boudouma, and Johanna Lofi. "Carbonate and silicate cementation of siliciclastic sediments of the New Jersey shelf (IODP Expedition 313): relation with organic matter diagenesis and submarine groundwater discharge." Geo-Marine Letters 37, no. 6 (April 8, 2017): 537–47. http://dx.doi.org/10.1007/s00367-017-0506-6.

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Kotthoff, U., D. R. Greenwood, F. M. G. McCarthy, K. Müller-Navarra, S. Prader, and S. P. Hesselbo. "Late Eocene to middle Miocene (33 to 13 million years ago) vegetation and climate development on the North American Atlantic Coastal Plain (IODP Expedition 313, Site M0027)." Climate of the Past 10, no. 4 (August 25, 2014): 1523–39. http://dx.doi.org/10.5194/cp-10-1523-2014.

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Abstract. We investigated the palynology of sediment cores from Site M0027 of IODP (Integrated Ocean Drilling Program) Expedition 313 on the New Jersey shallow shelf to examine vegetation and climate dynamics on the east coast of North America between 33 and 13 million years ago and to assess the impact of over-regional climate events on the region. Palynological results are complemented with pollen-based quantitative climate reconstructions. Our results indicate that the hinterland vegetation of the New Jersey shelf was characterized by oak–hickory forests in the lowlands and conifer-dominated vegetation in the highlands from the early Oligocene to the middle Miocene. The Oligocene witnessed several expansions of conifer forest, probably related to cooling events. The pollen-based climate data imply an increase in annual temperatures from ∼11.5 °C to more than 16 °C during the Oligocene. The Mi-1 cooling event at the onset of the Miocene is reflected by an expansion of conifers and mean annual temperature decrease of ∼4 °C, from ∼16 °C to ∼12 °C around 23 million years before present. Relatively low annual temperatures are also recorded for several samples during an interval around ∼20 million years before present, which may reflect the Mi-1a and the Mi-1aa cooling events. Generally, the Miocene ecosystem and climate conditions were very similar to those of the Oligocene. Miocene grasslands, as known from other areas in the USA during that time period, are not evident for the hinterland of the New Jersey shelf, possibly reflecting moisture from the proto-Gulf Stream. The palaeovegetation data reveal stable conditions during the mid-Miocene climatic optimum at ∼15 million years before present, with only a minor increase in deciduous–evergreen mixed forest taxa and a decrease in swamp forest taxa. Pollen-based annual temperature reconstructions show average annual temperatures of ∼14 °C during the mid-Miocene climatic optimum, ∼2 °C higher than today, but ∼1.5 °C lower than preceding and following phases of the Miocene. We conclude that vegetation and regional climate in the hinterland of the New Jersey shelf did not react as sensitively to Oligocene and Miocene climate changes as other regions in North America or Europe due to the moderating effects of the North Atlantic. An additional explanation for the relatively low regional temperatures reconstructed for the mid-Miocene climatic optimum could be an uplift of the Appalachian Mountains during the Miocene, which would also have influenced the catchment area of our pollen record.
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Cosgrove, Grace I. E., David M. Hodgson, Nigel P. Mountney, and William D. McCaffrey. "High-resolution correlations of strata within a sand-rich clinothem using grain fabric data, offshore New Jersey, USA." Geosphere 15, no. 4 (June 5, 2019): 1291–322. http://dx.doi.org/10.1130/ges02046.1.

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Abstract Trajectories of successive clinoform rollovers are widely applied to predict patterns of spatio-temporal sand distribution. However, the detailed internal architecture of individual clinothems is rarely documented. Understanding the textural complexities of complete topset-foreset-bottomset clinothem sequences is a key factor in understanding how and when sediment is transferred basinward. This study used high-resolution, core-based analyses of 267 samples from three research boreholes from quasi-coeval topset, foreset, and bottomset deposits of a single Miocene intrashelf clinothem recovered during Integrated Ocean Drilling Program (IODP) Expedition 313, offshore New Jersey, USA. Topset deposits were subdivided into three sedimentary packages based on grain character and facies analysis, consisting of upper and lower river-dominated topset process-regime packages separated by a middle wave- and storm-dominated process-regime package. Temporal variability in topset process regime exerts a quantifiable effect on grain character across the complete depositional profile, which was used here to correlate topset deposits with time-equivalent sedimentary packages in foreset and bottomset positions. River-dominated sedimentary packages have higher sand-to-mud ratios; however, the grain character of river-dominated sedimentary packages is texturally less mature than that of wave- and storm-dominated deposits. Differences in grain character between packages dominated by different process regimes increase basinward. The novel use of quantitative grain-character data allows intraclinothem time lines to be established at a higher resolution than is possible using chronostratigraphic techniques. Additionally, stratigraphic changes in grain character were used to refine the placement of the basal sequence boundary. These results challenge the idea that clinoform trajectories and stacking patterns are sufficient to describe spatio-temporal sand-body evolution across successive clinothems.
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Dissertations / Theses on the topic "IODP 313"

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Machado, Edimar Carvalho. "Comportamento Geoquímico do Iodo em Manguezal de Itacuruça-RJ." Universidade Federal Fluminense, 2004. http://www.bdtd.ndc.uff.br/tde_busca/arquivo.php?codArquivo=323.

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Conselho Nacional de Desenvolvimento Cientifico e Tecnológico
Coordenação de Aperfeiçoamento de Pessoal de Nível Superior
O presente estudo utilizou radiotraçador para acompanhar a especiação do iodo em amostras de água de manguezal durante experimentos de incubação, em laboratório, onde o efeito da filtração, utilizando filtro de porosidade 0,22 mm, sobre a conversão entre iodeto e iodato foi verificado. Após 61 dias de incubação, os resultados indicaram não haver diferença significativa na conversão de iodato a iodeto entre as amostras filtradas e não filtradas (44,6 9,7%). Foi observada pequena retenção do iodato nos filtros (2% nas amostras não filtradas e 0,5% nas amostras esterilizadas). Não houve, também, diferença na oxidação do iodeto entre as amostras. Contudo, observou-se maior retenção do radiotraçador no material particulado que chegou a reter 7% do iodeto nas amostras não filtradas. Estudou-se ainda, a cinética de remoção de iodeto e iodato da coluna d`água pelo sedimento e o enriquecimento deste elemento no sedimento em diferentes condições de óxi-redução na interface água-sedimento. A remoção de iodeto e iodato da coluna d`água obedeceu a uma cinética de 1 ordem e seu enriquecimento na camada superficial do sedimento ocorreu tanto em condições óxicas quanto em condições anóxicas, porém, em condições óxicas, esta remoção foi mais rápida e houve maior acúmulo do radiotraçador na camada superficial do sedimento, indicando assim, que os processos de remoção e acúmulo do iodo são dependentes do Eh. Observou-se, ainda, desprendimento de até 9 vezes mais iodo retido no sedimento em condições anóxicas do que em condições óxicas. Em condições anóxicas, retornou até 27% do iodo retido no sedimento para a coluna d`água, enquanto, em condições óxicas, este retorno chegou apenas a 3%. Isso demonstra que o sedimento, em condições anóxicas, pode agir como fonte deste elemento para a coluna d`água. Testemunhos com remoção da matéria orgânica e dos microorganismos mostraram pequena diferença na cinética de remoção e no acúmulo de iodato comparados aqueles que não sofreram tratamento, sugerindo, um papel secundário da matéria orgânica e dos microorganismos nos processos de enriquecimento de iodo pelos sedimentos.
This study used radiotracers to investigate the iodine speciation in mangrove waters in incubation experiments in laboratory, on which the role of biological and chemical processes were evaluated. After 61 days of incubation, results did not indicate a significant difference between filtered and unfiltered samples for iodate convertion to iodide (44.6 9.7%). It was observed a low retention of iodate in the filters (2% in unfiltered samples and 0.5% in sterilized samples). However, it was observed a greater radiotracer retention by particulate matter (up to 7% of iodide in unfiltered samples). The kinetics of iodide and iodate removal from the water column by sediments and the enrichment of iodine within sediments under different redox conditions near the water-sediment interface was also investigated. Iodide and iodate removal from water followed a first-order kinetics and their enrichment in surface sediment layers occurred in oxic and ano xic conditions. This the removal was faster and the sediment enrichment was greater in oxic conditions, indicating that both are redox-dependent. After iodine removal from the water column, it was observed an iodine release 9 times greater from sediments in anoxic conditions than in oxic conditions. In anoxic conditions there was a iodine return to the water column up to 27%, whereas in oxic conditions this return was up to 3%. This demonstrates that anoxic sediments be a source of iodine to the water column. Organic matter- free, sterilized sediments showed a low difference for the kinetics of iodate removal, suggesting an secondary role of organic matter and microorganisms in the process of iodine enrichment by sediments.
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Nunes, Sonia Carvalho. "IMPLICAÇÕES DO CÂNCER DE TIREÓIDE NA QUALIDADE DE VIDA DE INDIVÍDUOS QUE FAZEM TRATAMENTO COM IODO-131 E SEUS FAMILIARES." Pontifícia Universidade Católica de Goiás, 2011. http://localhost:8080/tede/handle/tede/3139.

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Made available in DSpace on 2016-08-10T10:56:05Z (GMT). No. of bitstreams: 1 SONIA CARVALHO NUNES.pdf: 3517823 bytes, checksum: 40ac535818499c2006588bb3bb0da59e (MD5) Previous issue date: 2011-05-13
This study has the goal to evaluate the quality of life of patients and companions who are treated with Iodine-131, in other words radiotherapy. In order to identify and associate the main factors that affect quality of life for both patients and the companion during the treatment. The study population consisted of 56 individuals, among them 32 are carriers of Differentiated Thyroid Cancer and 24 companions of the patients are among the companions are: children, spouse (a), other relatives and friends. Were administered two questionnaires, the first refers to the sociodemographic and lifestyle variables, and the second by the specific instrument of the World Health Organization (WHO) to assess quality of life, called WHOQOL-bref. The study was conducted at the Centro Brasileiro de Medicina Nuclear e Imagem Molecular em Goiânia-Go, in the period September to December 2010. It was used two methodological approaches: a quantitative relationship to the organization of the questionnaire results in percentage form represented in tables, and other qualitative study using Grounded Theory for interpreting the reports of caregivers and patients before and after hospitalization in the therapeutic room. From the participants' reports, of the results of questionnaires that were applied and understandings that were built during the research, using Grounded Theory, it was identified the major categories that affect the quality of life of both patients and their carers. The main categories found were: adverse elements in the context of treatment, emotional impact of diagnosis and treatment, problems of coping and coping factors that favor. Furthermore, both patients and companions presented suggestions during treatment that in their opinion would improve the quality of life. The quantitative analysis revealed that most patients and caregivers are satisfied with the quality of life. The results are discussed with the intention of better understanding the perspective of the patient and companion on the factors that may help to improve the quality of life, in order to mitigate the problems that appeared during treatment.
O presente estudo tem o objetivo de avaliar a qualidade de vida de pacientes e acompanhantes que fazem tratamento de Câncer Diferenciado da Tireóide utilizando radioiodoterapia com Iodo-131. Tem o intuito de identificar e associar os principais fatores que interferem na qualidade de vida tanto do paciente como do acompanhante no decorrer do tratamento. A população de estudo foi constituída de 56 indivíduos, dentre eles 32 portadores do Câncer Diferenciado da Tireóide e 24 acompanhantes dos mesmos. Entre os acompanhantes estão: filhos, pais, esposo (a), amigos e outros parentes. Foram aplicados dois questionários fechados, sendo o primeiro referente as variáveis sociodemográficas e estilo de vida, e o segundo referente a instrumento específico da Organização Mundial de Saúde (OMS), para avaliação da qualidade de vida, denominado WHOQOL-bref. O estudo foi realizado no Centro Brasileiro de Medicina Nuclear e Imagem Molecular em Goiânia-GO, no período de setembro a dezembro de 2010. Foram utilizadas duas abordagens metodológicas: uma quantitativa com a organização dos resultados dos questionários, em forma de porcentagem representado nas tabelas, e a outra qualitativa, utilizando a Grounded Theory para a interpretação dos relatos dos acompanhantes e pacientes antes e após a internação no quarto terapêutico. A partir do relato dos participantes, dos resultados dos questionários que foram aplicados e dos memorandos que foram construídos no decorrer da pesquisa e utilizando a Grounded Theory foram identificadas as principais categorias que interferem na qualidade de vida tanto dos pacientes como de seus acompanhantes. As principais categorias encontradas foram: elementos adversos no contexto do tratamento, impacto emocional de diagnostico e tratamento, problemas de enfrentamento e elementos que o favorecem. Além disso, tanto os pacientes como acompanhantes apresentaram sugestões no decorrer do tratamento, que na opinião deles poderia melhorar a qualidade de vida. A análise quantitativa mostrou que a maioria dos pacientes e acompanhantes estão satisfeitos com a qualidade de vida. Os resultados são discutidos com a intenção de compreender melhor a perspectiva do paciente e do acompanhante sobre os fatores que podem auxiliar na melhoria da qualidade de vida, com o intuito de amenizar os problemas que surgiram no decorrer do tratamento.
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Martin-Dexmier, Sophie. "Synthèse et réactivité des fluorovinylsilanes." Paris 6, 1986. http://www.theses.fr/1986PA066319.

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Synthèse des difluorovinyl silanes. Mise au point d'une des meilleures voies d'accès aux composés suivants : difluoro-1,2 alcènes, chloro-1 fluoro-2 alcènes, alcènes difluorés substitués et cétones alpha, beta -éthyléniques alpha, beta -difluorées.
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Polat, Faik Ozcan. "Core-seismic correlation and sequence stratigraphy at IODP Expedition 317 drillsites, Canterbury Basin, New Zealand." 2012. http://hdl.handle.net/2152/20037.

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High rates of Neogene sediment influx to the offshore Canterbury Basin resulted in preservation of a high-resolution record of seismically resolvable sequences (~0.1-0.54 my periods). Subsequent sequence development was strongly influenced by submarine currents. This study focuses on correlating seismically interpreted sequence boundaries and sediment drifts architectures beneath the modern shelf and slope with sediment facies observed in cores from shelf Site U1351 and slope Site U1352 drilled by Integrated Ocean Drilling Program (IODP) Expedition 317. A traveltime-depth conversion was created using sonic and density logs and is compared with two previous traveltime-depth conversions for the sites. Eleven large elongate drifts were interpreted prior to drilling. Two new small-scale plastered slope drifts in the vicinity of the IODP sites, together with sediment waves drilled at Site U1352, have been interpreted as part of this study. Lithologic discontinuity surfaces and transitions together with associated sediment packages form the basis of identifying sequences and sequence boundaries in the cores. Contacts and facies were characterized using shipboard core descriptions, emphasizing grain-size contrasts and the natures of the lower and upper contacts of sediment packages. Lithologic surfaces in cores from sites U1351- (surfaces S1-S8) and U1352- (surfaces S1-S6) correlate with early Pleistocene to recent seismic sequence boundaries U12-U19 and U14-U19, respectively. The limited depths achieved by downhole logging, in particular sonic and density logs, together with poor recovery in the deeper section did not allow correlation of older lithologic surfaces. Slope Site U1352 experienced a complex interplay of along-strike and downslope depositional processes and cores provide information about the principal facies forming sediment waves. The general facies are fine-grained mud rich sediment interbedded decimeter-centimeter thick sand and sandy mud. Core evidence for current activity is reinforced at larger scale by seismic interpretations of sediment waves and drifts.
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Wang, Jiasheng, Qi Chen, Qing Wei, Xiaoqin Wang, Qing Li, and Yuya Gao. "AUTHIGENIC PYRITES AND THEIR STABLE SULFUR ISOTOPES IN SEDIMENTS FROM IODP 311 ON CASCADIA MARGIN, NORTHEASTERN PACIFIC." 2008. http://hdl.handle.net/2429/1370.

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In order to understand the response of authigenic minerals to the gas hydrate geo-system, various authigenic pyrites were picked out under Zeiss Microscope and their S isotopes were analyzed later from 652 sediments samples at intervals of about 1.5m recovered from all 5 sites of Integrated Ocean Drilling Program (IODP) Expedition 311 on Cascadia Margin, northeastern Pacific. SEM photos of picked pyrites exhibit various aggregation features mainly in forms of strawberry, pillar/rod and dumbbell in sizes from 200 m to 1000m. Typical cubic pyrite crystals could be seen under smaller scale SEM photos. Most δ34S values in Site U1325 at the west deeper water location of IODP 311 show negative values low to -33.964‰ CDT, distinctly contrasted to the δ34S in Site U1329 at the east shallower location having much more positive values up to 28.29‰ CDT. At the cold venting position assigned as Site U1328 the δ34S values show strong negative values in the upper part of sediments column above 135 mbsf (meter below sea floor), increasing gradually with the depth from -35.83‰ CDT to -1.32‰ CDT, and then display many positive excursions up to 32.49‰ CDT below 135 mbsf, which is significantly distinguished from the values in nearby non-cold venting Site U1327 having much less positive excursions in the lower part of column below 110 mbsf. In all sites a general negative δ34S excursion occur in the upper part of sediments columns above 30~35 mbsf except in Site U1328 having more depth, indicating the potential current sulfate methane interface (SMI) activity zones. Distinct positive δ34S excursions up to the highest δ34S value 53.65‰ CDT from strawberry pyrites aggregations might indicate that sulfide products by AOM probably inherit completely the sulfate having high δ34S value and no sulfate was left after AOM at a high methane flux under gas hydrate geological background.
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Szidat, Sönke [Verfasser]. "Iod-129 : Probenvorbereitung, Qualitätssicherung und Analyse von Umweltmaterialien / von Sönke Szidat." 2000. http://d-nb.info/960643281/34.

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Schmidt, Annette Christine [Verfasser]. "129I und stabiles Iod in Umweltproben : Qualitätskontrolle von Analysenmethoden und Untersuchungen zur Radioökologie und zur retrospektiven Dosimetrie / von Annette Christine Schmidt." 1998. http://d-nb.info/954459563/34.

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Book chapters on the topic "IODP 313"

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Riedel, Michael, Timothy S. Collett, Martin Scherwath, John W. Pohlman, Roy Hyndman, and George Spence. "Northern Cascadia Margin Gas Hydrates—Regional Geophysical Surveying, IODP Drilling Leg 311 and Cabled Observatory Monitoring." In World Atlas of Submarine Gas Hydrates in Continental Margins, 109–20. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-81186-0_8.

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Siaudvytyte, Lina. "Interactions Between IOP, ICP, OPP." In Biophysical Properties in Glaucoma, 31–34. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-98198-7_7.

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Fink, Hiske G., Michael Strasser, Miriam Römer, Martin Kölling, Ken Ikehara, Toshiya Kanamatsu, Dominik Dinten, et al. "Evidence for Mass Transport Deposits at the IODP JFAST-Site in the Japan Trench." In Submarine Mass Movements and Their Consequences, 33–43. Cham: Springer International Publishing, 2013. http://dx.doi.org/10.1007/978-3-319-00972-8_4.

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Jasser, Jasser, Hua Ming, and Mohamed A. Zohdy. "Situation-Awareness in Action: An Intelligent Online Learning Platform (IOLP)." In Lecture Notes in Computer Science, 319–30. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-58077-7_25.

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Stoeva, M., and R. Vetter. "Radiation Protection – A Global View. A New IOMP-IRPA Initiative." In XIV Mediterranean Conference on Medical and Biological Engineering and Computing 2016, 950–53. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-32703-7_185.

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Kunkel, Julian, Jay Lofstead, and Colin McMurtrie. "HPC I/O in the Data Center Workshop (HPC-IODC)." In Lecture Notes in Computer Science, 127–31. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-67630-2_11.

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"Expedition 313 summary." In Proceedings of the IODP. Integrated Ocean Drilling Program, 2010. http://dx.doi.org/10.2204/iodp.proc.313.101.2010.

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Inwood, J., A. McGrath, S. Morgan, M. Norry, S. Davies, and H. Foster. "Data report: Expedition 313 elemental data from X-ray fluorescence scanning and measurements on core samples." In Proceedings of the IODP. International Ocean Discovery Program, 2019. http://dx.doi.org/10.2204/iodp.proc.313.203.2019.

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Ando, H., M. Oyama, and F. Nanayama. "Data report: grain size distribution of Miocene successions, IODP Expedition 313 Sites M0027, M0028, and M0029, New Jersey shallow shelf." In Proceedings of the IODP. Integrated Ocean Drilling Program, 2014. http://dx.doi.org/10.2204/iodp.proc.313.201.2014.

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Inwood, J. "Data report: interpretation of cored intervals with greater than one hundred percent core recovery: IODP Expedition 313 used as an example methodology." In Proceedings of the IODP. International Ocean Discovery Program, 2018. http://dx.doi.org/10.2204/iodp.proc.313.202.2018.

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Conference papers on the topic "IODP 313"

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Seth, V., V. Srivardhan, and S. Maiti. "Evaluation of Formation Shaliness Using Factor Analysis of site-U1344A of IODP Expedition 323 in the Bering Sea." In 77th EAGE Conference and Exhibition 2015. Netherlands: EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201412469.

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2

Shinmoto, Y. "A Case Study on Downhole Measurement to Monitor Drilling Hazards in Integrated Ocean Drilling Program (IODP) Expedition 314." In OCEANS 2008 MTS/IEEE Kobe Techno-Ocean. IEEE, 2008. http://dx.doi.org/10.1109/oceanskobe.2008.4530994.

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Harbour, Thomas A., and Beth E. Caissie. "FINE-SCALE ANALYSIS OF LAMINATED SEDIMENTS FROM MARINE ISOTOPE STAGE 11 (425 KA) IN THE BERING SEA, IODP EXPEDITION 323, SITE U1345." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-313073.

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4

Phillips, Stephen, Joel E. Johnson, Joel E. Johnson, William C. Clyde, William C. Clyde, Wei-li Hong, Wei-li Hong, et al. "TRACKING DIAGENETIC ALTERATION OF MAGNETIC SUSCEPTIBILITY IN METHANE HYDRATE-BEARING MARINE SEDIMENTS OF THE CASCADIA MARGIN (ODP LEG 204 AND IODP EXPEDITION 311)." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357325.

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5

Abanum, Andrew Monday, Ibidabo David Alebere, and Chinemerem Patricks-E. "Determinants of IOGP Life-Saving Rules Compliance Among Nigerian Petroleum Industry Workers." In SPE Nigeria Annual International Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/208227-ms.

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Abstract:
Abstract Life-saving rules (LSRs) are a set of defined rules that support and complement general site-specific safety rules and procedures (SRPs). LSRs are popular in the oil & gas (O&G) industry and are part of the safety management system framework designed to prevent incidents in the workplace. Complying with LSRs ensures its intent of incident prevention, drives the goal of creating decent work, economic growth and sustainable development. With the continuum of incidents in the industry, total compliance with LSRs and SRPs still remains a mirage. Even though the introduction of LSRs in the O&G caused a paradigm shift from fair to better safety performance, incident investigations continue to unveil cases of violations/non-compliance. In the space of continuous improvement, it becomes expedient to determine possible causes of these LSRs and SRPs non-compliance, with a view to nipping the causal factors in the bud. A descriptive cross-sectional study was conducted to determine the factors affecting the level of workers compliance with IOGP LSRs in selected O&G companies operating in Delta State, Nigeria. The research recruited 317 sharp end workers and selected leaders, through a multistage sampling technique. A semi-structured, self-administered questionnaire was used as instrument for data collection. The study in its findings was able to elicit numerous compliance determinants arising from socio-demography, occupational and organisational factors. These factors are barriers to strengthen if the goal of total compliance and zero incident must be achieved in the workplace. The study recommends that management should comply with Thomas Legge's aphorisms 1 & 4 on SRPs and design training programmes for employees to be imparted with requisite knowledge needed for compliance, commit to safety and lead a positive safety culture to drive continuous improvement. Furthermore, there is the need to pursue total compliance with LSRs, SRPs and any site-specific safety rules to achieve zero incidents in the O&G industry.
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Wang, Stephanie, Nolan Maloney, Ruth Hsiao, Mariko Limpar, Naohiko Ikegaki, and Xao X. Tang. "Abstract 2875: Meta-iodo-benzylguanidine (MIBG) is a MYCN/MYC destabilizer that specifically targets neural crest derived tumors." In Proceedings: AACR 103rd Annual Meeting 2012‐‐ Mar 31‐Apr 4, 2012; Chicago, IL. American Association for Cancer Research, 2012. http://dx.doi.org/10.1158/1538-7445.am2012-2875.

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