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Letteratura scientifica selezionata sul tema "Igneous"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 5 marzo 2023

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Articoli di riviste sul tema "Igneous"

1

Hellawell, Jo. "Igneous triangle". Nature Geoscience 8, n. 12 (27 novembre 2015): 904. http://dx.doi.org/10.1038/ngeo2614.

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2

Leeman, William P. "Igneous petrogenesis". Geochimica et Cosmochimica Acta 61, n. 10 (maggio 1997): 2147. http://dx.doi.org/10.1016/s0016-7037(97)83223-1.

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3

Burley, Brian J. "Igneous petrology". Geochimica et Cosmochimica Acta 52, n. 3 (marzo 1988): 798. http://dx.doi.org/10.1016/0016-7037(88)90345-6.

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4

Helz, R. T. "Igneous petrology". Journal of Volcanology and Geothermal Research 24, n. 3-4 (maggio 1985): 361–62. http://dx.doi.org/10.1016/0377-0273(85)90080-0.

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5

Potter, Joanna, Andrew H. Rankin, Peter J. Treloar, Valentin A. Nivin, Wupao Ting e Pei Ni. "A preliminary study of methane inclusions in alkaline igneous rocks of the Kola igneous province, Russia: implications for the origin of methane in igneous rocks". European Journal of Mineralogy 10, n. 6 (1 dicembre 1998): 1167–80. http://dx.doi.org/10.1127/ejm/10/6/1167.

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6

Coffin, Millard F., e Clive Neal. "Large igneous provinces". Eos, Transactions American Geophysical Union 88, n. 47 (20 novembre 2007): 505. http://dx.doi.org/10.1029/2007eo470009.

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7

Coffin, Millard F., e Olav Eldholm. "Large Igneous Provinces". Scientific American 269, n. 4 (ottobre 1993): 42–49. http://dx.doi.org/10.1038/scientificamerican1093-42.

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8

Le Maitre, R. W. "Alkaline Igneous rocks". Geochimica et Cosmochimica Acta 52, n. 9 (settembre 1988): 2343. http://dx.doi.org/10.1016/0016-7037(88)90137-8.

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9

De Wit, Maarten J. "Alkaline igneous rocks". Lithos 24, n. 1 (dicembre 1989): 81–82. http://dx.doi.org/10.1016/0024-4937(89)90017-0.

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10

Reynolds, Owen. "Ambiguous Igneous Rocks". Archives of Dermatology 143, n. 1 (1 gennaio 2007): 115. http://dx.doi.org/10.1001/archderm.143.1.118.

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Tesi sul tema "Igneous"

1

Jolly, Richard J. H. "Mechanisms of igneous sheet intrusion". Thesis, University of Southampton, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.242207.

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2

Esfarjani, H. R. "Engineering properties of basic igneous rocks". Thesis, University of Newcastle Upon Tyne, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.374739.

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3

Student, James John. "Silicate Melt Inclusions in Igneous Petrogenesis". Diss., Virginia Tech, 2002. http://hdl.handle.net/10919/28719.

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Silicate melt inclusions are ubiquitous in quartz phenocrysts, yet there are few studies of such inclusions from porphyry copper systems. A melt inclusion forms when magma is trapped in a growing phenocryst. If a phenocryst is able to preserve the original parent magma, then accurate information can be obtained for ancient volcanic systems. In recent igneous systems, melt inclusions are commonly preserved as optically clear homogeneous glass representative of magma stored at depth before eruption. Melt inclusions are difficult to recognize in quartz phenocrysts from porphyry copper system because they are crystalline and hidden by exsolved magmatic volatiles. The inclusions range in size from less than 5 to over 150 Î¼m. In order to evaluate the magmatic contribution to economic mineralization, we conducted three separate studies to determine whether or not crystallized melt inclusions preserve representative samples of magma. The first study modeled the phase relationships that occur during equilibrium crystallization and melting of haplogranite magma trapped in quartz. Results from the model are similar to observations made during the heating of crystallized melt inclusions from porphyry copper systems. It is necessary to re-melt the crystal and volatile phases before chemical analysis. Micro-explosions caused by heating resulted in the loss of important chemical components. Our second study evaluated several microthermometric heating procedures using synthetic melt inclusions trapped at conditions similar to those inferred for porphyry copper systems. A synthetic hydrous melt was saturated with saline hydrothermal solutions allowing both melt and aqueous fluids to be trapped in quartz. Based on microthermometric measurements from these coeval melt and aqueous fluid inclusions we were able to predict the known trapping temperature and pressure of formation. This technique can be applied to natural samples to constrain trapping pressures and temperatures. It was found that slower heating rates could be used to avoid overheating and that heating under a confining pressure greatly minimizes the decrepitation of inclusions. The third study examined the copper concentrations in melt inclusions from the Red Mountain, Arizona porphyry copper system. Older andesite magma contains pyroxene with melt inclusions of higher copper concentrations compared to melt inclusions in quartz from quartz latite. The higher water concentrations in crystallized melt inclusions in the quartz, and abundant aqueous fluid inclusions indicates that the exsolution of water from the magma occurred prior to the trapping of melt inclusions in quartz. The lower water concentrations and the absence of aqueous fluid inclusions indicates that the andesite never reached the stage of water exsolution. The results obtained here are consistent with models that suggest that copper is extracted from the melt by saline magmatic fluids, producing a metal-charged hydrothermal solution and leaving behind a metal-depleted melt and serves to identify the potential contribution of melt inclusion studies to constrain the origin of ore metals in porphyry copper deposits.
Ph. D.

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4

Pattison, Christopher Ian. "Igneous intrusions in the Bowen Basin". Thesis, Queensland University of Technology, 1990. https://eprints.qut.edu.au/35967/1/35967_Pattison_1990.pdf.

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Igneous intrusions, in the form of stocks, sills and dykes are abundant in the Bowen Basin. They are predominantly Early Cretaceous in age, exclusively epizonal in origin and range in composition from dolerite to granodioriteldacite. All rock units within the basin, up to and including the Clematis Group, are intruded to some degree. This study assesses the distribution, form, petrology and mode of emplacement of plutons, igneous sills and dykes occurring in the Bowen Basin, and considers their relationship to the prevailing structure. The tectonic implications of the findings are then assessed. Igneous sills occur in two geographically distinct domains, one in the northern Bowen Basin and the other in the central Bowen Basin. The sills emanated from pre-existing, north to north-northwest trending reverse faults, and preferentially intruded coal seams. The boundaries to sill intrusion are marked by major northeast trending basement structures. These basement structures occur at regular intervals throughout the basin, and correspond with the localisation of plutonic and dyke activity, anomalous structural disturbance, and changes in the gross structure of the basin. They are interpreted as transfer faults that were inherited from an Early Permian, basin-forming extensional episode. Petrological evidence indicates that the plutons and sills occurring in the northern Bowen Basin are petrogenetically related, and that a progressive variation in their chemistry occurs across the axis of the basin from east to west. Intrusions in the east belong to the calc-alka1ine rock suite, while those in the west belong to the syenitic suite. This transition is inte1preted in terms of increased crustal contamination as the magma migrated from a source area to the east along a buried, shallow-dipping detachment surface that extends under the basin. This detachment was inherited from the above mentioned extensional phase and is intimately linked to structures that penetrate up-section through the basin succession. Reactivation of the transfer faults during the Early Cretaceous initiated the emplacement of dykes, and the synchronous development of northeast trending normal and wrenchstyle faults. The dykes exhibit characteristics that indicate they were self-propagating, and can be regarded as good palaeostress indicators. This phase corresponded with a major compressional event that involved the reactivation of pre-existing thrust structures, deformation of the Folded Zone and eastern margins of the Nebo Synclinorium and Mimosa Syncline, and the rapid preferential uplift of the central Bowen Basin region.

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5

Jurinski, Joseph B. "Petrogenesis of the Moosehorn igneous complex, Maine". Thesis, This resource online, 1990. http://scholar.lib.vt.edu/theses/available/etd-04072010-020130/.

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6

Reichow, Marc K. "Permo-Triassic igneous rocks of Siberia, Russia". Thesis, University of Leicester, 2004. http://hdl.handle.net/2381/7669.

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Widespread basaltic volcanism occurred in the region of the West Siberian Basin (WSB) and the Taimyr Peninsula in central Russia, and voluminous A-type magmatism within the Mongolian-Transbaikalian belt in southeast Siberia, during Permo-Triassic times. New 40Ar/39Ar age determinations on plagioclase grains from deep boreholes in the WSB reveal that the basalts were erupted at ~250 million years ago. This is synchronous with the main period of the Siberian Traps volcanism, which was located farther east. The age and geochemical data presented confirm that the WSB basalts are part of the Siberian Traps, and at least double the confirmed area of the volcanic province as a whole. The larger area of volcanism strengthens the link between the volcanism and the end-Permian mass extinction. Furthermore, it is argued that the WSB and Taimyr basalts are genetically related to the Siberian Traps basalts, especially the Nadezhdinsky Suite found at Noril’sk. This suite immediately preceded the main pulse of volcanism that extruded lava over large areas of the Siberian Craton. Magma volume and timing constraints strongly suggest that a mantle plume was involved in the formation of the Earth’s largest continental flood basalt province. The Mongolian-Transbaikalian granitoid belt covers over 600,000 km2 with over 350 single A-type plutons. New U-Pb geochronological data presented here demonstrate that no plutonic complex dated is 250 Ma old. Although mantle-derived material played a prominent role in the granitoid generation, these melts may have been generated by processes other than decompressional melting within the head of a mantle plume. The new U-Pb ages and other observations contradict the idea of a relation between the Siberian plume and magmatic activity in the territory of Transbaikalia. An alternative preferred model inducing up rise of asthenospheric material includes slab break-off after a long period of subduction.

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7

Rainey, Michelle M. "Microfractures in the weathering of igneous rock". Thesis, Queen's University Belfast, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239231.

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8

Singletary, Steven J. (Steven James) 1973. "Igneous processes of the early solar system". Thesis, Massachusetts Institute of Technology, 2003. http://hdl.handle.net/1721.1/58444.

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Thesis (Ph. D. in Geochemistry)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, February 2004.
Includes bibliographical references.
Experimental, petrographic and numerical methods are used to explore the igneous evolution of the early solar system. Chapters 1 and 2 detail the results of petrographic and experimental studies of a suite of primitive achondritic meteorites, the ureilites. The first chapter presents data that reveal correlations between mineral modal proportions and mineral chemistry that are used to guide experiments and models of ureilite petrogenesis. Chapter 2 details and applies the experimental results to describe ureilite petrogenesis as the result of progressive heating of a primitive carbon-rich body. The experiments place temperature and depth constraints on uteilite formation of 1100 to 13000C and 5 to 13 MPa - equivalent to the central pressure of an asteroid with a radius of 130 km. Chapter 3 reports the results of melting experiments of Allende carbonaceous chondrite at temperatures and pressures that would be expected on small bodies in the early solar system (up to 1300⁰C and 2.5 to 15 IPa) heated by decay of short lived isotopes. The results are then applied to ureilite petrogenesis and assembly of larger planetary bodies. The final chapter is an experimental study to test a hybridized source region for the high titanium lunar ultramafic glasses. Two models are presented that invoke either a heterogeneous source region or sinking and reaction of an ultramafic, titanium rich magma with underlying mantle regions.
by Steven J. Singletary.
Ph.D.in Geochemistry

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9

Marchand, Kateri. "Étude d'éléments structuraux dans la demie nord du Canton de McKenzie, Chibougamau /". Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1990. http://theses.uqac.ca.

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10

Mainville, Michèle. "Les komatiites et tholéiites à la base du groupe de baby, Témiscamingue /". Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1994. http://theses.uqac.ca.

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Libri sul tema "Igneous"

1

Hall, Anthony. Igneous petrology. Harlow, Essex, England: Longman Scientific & Technical, 1987.

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2

Zhaonai, Li, Qi Jianzhong e Zhang Zhaochong. Igneous Petrology. London: CRC Press, 2021. http://dx.doi.org/10.1201/9780429070877.

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3

Le Maitre, R. W., A. Streckeisen, B. Zanettin, M. J. Le Bas, B. Bonin e P. Bateman, a cura di. Igneous Rocks. Cambridge: Cambridge University Press, 2002. http://dx.doi.org/10.1017/cbo9780511535581.

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4

Wilson, Marjorie. Igneous Petrogenesis. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-010-9388-0.

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Wilson, Marjorie, a cura di. Igneous Petrogenesis. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-1-4020-6788-4.

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6

Igneous petrogenesis. London: Unwin Hyman, 1989.

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7

Igneous petrology. 3^a ed. Sudbury, Mass: Jones and Bartlett Publishers, 2007.

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8

Oxlade, Chris. Igneous rocks. Chicago, Ill: Heinemann Library, 2011.

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9

A, Hall. Igneous petrology. Harlow: Longman, 1987.

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10

Igneous rock. Oxford: Raintree, 2008.

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Capitoli di libri sul tema "Igneous"

1

de Oliveira Frascá, Maria Heloisa Barros, e Eliane Aparecida Del Lama. "Igneous Rocks". In Selective Neck Dissection for Oral Cancer, 1–6. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-12127-7_166-1.

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2

Okrusch, Martin, e Hartwig E. Frimmel. "Igneous Rocks". In Springer Textbooks in Earth Sciences, Geography and Environment, 249–74. Berlin, Heidelberg: Springer Berlin Heidelberg, 2020. http://dx.doi.org/10.1007/978-3-662-57316-7_13.

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3

Chantraine, J., B. Auvray e D. Rabu. "Igneous Activity". In Pre-Mesozoic Geology in France and Related Areas, 111–25. Berlin, Heidelberg: Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-84915-2_6.

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4

Fernandes, Isabel, Helena Martins, Maria dos Anjos Ribeiro, Fernando Noronha, Maarten A. T. M. Broekmans e Ian Sims. "Igneous Rocks". In Petrographic Atlas: Characterisation of Aggregates Regarding Potential Reactivity to Alkalis, 9–41. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-017-7383-6_2.

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5

Arndt, Nicholas. "Igneous Rock". In Encyclopedia of Astrobiology, 1. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_773-3.

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Arndt, Nicholas. "Igneous Rock". In Encyclopedia of Astrobiology, 1182–83. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_773.

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7

Zhang, Jianfang, Chaohui Zhu, Longwu Wang, Xiaoliang Cai, Ruijun Gong, Xiaoyou Chen, Jianguo Wang, Mingguang Gu, Zongyao Zhou e Yuandong Liu. "Igneous Rocks". In The China Geological Survey Series, 173–255. Singapore: Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-1788-4_3.

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Arndt, Nicholas. "Igneous Rock". In Encyclopedia of Astrobiology, 805. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_773.

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9

Corretge, L. G., O. Suarez e G. Galan. "Igneous Rocks". In Pre-Mesozoic Geology of Iberia, 115–28. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-83980-1_10.

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10

Sanchez Carretero, R., L. Eguiluz, E. Pascual e M. Carracedo. "Igneous Rocks". In Pre-Mesozoic Geology of Iberia, 292–313. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-83980-1_19.

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Atti di convegni sul tema "Igneous"

1

F. Coffin, Millard. "Large Igneous Province". In 5th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.299.297.

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2

Li, Shaoxuan, Xiaobo Huang, Yu Xiong, Kai Su e Yongchao Zhu. "Mechanism Analysis and Prediction of Lost Circulation in Igneous Formation: A Case Study from B Oilfield, Bohai Bay Basin, China". In Offshore Technology Conference. OTC, 2022. http://dx.doi.org/10.4043/31764-ms.

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Abstract Volcanic reservoirs are gradually becoming an important target for exploration and development in Bohai Bay, China. At the same time, the igneous formation is more prone to lost circulation than the conventional sedimentary formation. On the one hand, there is a lack of understanding of the mechanism of drilling fluid leakage in igneous formation; on the other hand, there is a lack of measured data on the leakage pressure of igneous formation. As a result, the risk prompt for well leakage in igneous formation before drilling is insufficient, and there is a lack of targeted plugging measures in case of well leakage during drilling, resulting in the original formation being polluted by mud and even abandoned by the project, which restricts the effectiveness of exploration and development of the oilfield. In response to the above problems, firstly, innovatively carry out research on the loss mechanism of igneous rock to help drilling engineering professionals formulate specific plugging measures for special lithological formations. Then summarize the igneous rock leakage laws of different lithofacies, and quantitatively evaluate the pressure bearing capacity of different lithofacies. Finally, the fine identification and characterization of pre-drilling igneous facies are carried out based on the difference of seismic reflection characteristics. Comprehensively apply the above research results to quantitatively predict the risk of lost circulation before drilling in B oilfield in Bohai Bay Basin to avoid lost circulation accidents.

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3

Li, Shaoxuan, Xiaobo Huang, Yu Xiong, Kai Su e Yongchao Zhu. "Mechanism Analysis and Prediction of Lost Circulation in Igneous Formation: A Case Study from B Oilfield, Bohai Bay Basin, China". In Offshore Technology Conference. OTC, 2022. http://dx.doi.org/10.4043/31764-ms.

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Abstract Volcanic reservoirs are gradually becoming an important target for exploration and development in Bohai Bay, China. At the same time, the igneous formation is more prone to lost circulation than the conventional sedimentary formation. On the one hand, there is a lack of understanding of the mechanism of drilling fluid leakage in igneous formation; on the other hand, there is a lack of measured data on the leakage pressure of igneous formation. As a result, the risk prompt for well leakage in igneous formation before drilling is insufficient, and there is a lack of targeted plugging measures in case of well leakage during drilling, resulting in the original formation being polluted by mud and even abandoned by the project, which restricts the effectiveness of exploration and development of the oilfield. In response to the above problems, firstly, innovatively carry out research on the loss mechanism of igneous rock to help drilling engineering professionals formulate specific plugging measures for special lithological formations. Then summarize the igneous rock leakage laws of different lithofacies, and quantitatively evaluate the pressure bearing capacity of different lithofacies. Finally, the fine identification and characterization of pre-drilling igneous facies are carried out based on the difference of seismic reflection characteristics. Comprehensively apply the above research results to quantitatively predict the risk of lost circulation before drilling in B oilfield in Bohai Bay Basin to avoid lost circulation accidents.

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4

Baker, Don R. "MODELING NUCLEATION DELAY IN IGNEOUS SYSTEMS". In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-316863.

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5

Anuka, Agnes, Celestine Udie e Grace Aquah. "Prospects, Challenges and Way Forward in the Use of Hydraulic Fracturing For Oil and Gas Production From Igneous Rocks". In SPE Nigeria Annual International Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/207106-ms.

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Abstract Commercial accumulation of hydrocarbons occurs mostly in sedimentary rocks due to their high porosity and permeability. Increased global energy demand has necessitated the need for unconventional methods of oil production. The world is gradually moving away from reliability on conventional oils. The need to ensure global energy sustainability has necessitated an urgent diversion to unconventional oils. In recent times, hydrocarbon accumulations have been found in igneous rocks. Their low porosity and permeability however prevents commercial production as oil and gas found in these rocks will not flow. Hydraulic fracturing is useful in increasing rock porosity as it involves the breaking of rocks to allow oil and gas trapped inside to flow to producing wells. This method is useful in developing unconventional resources such as oil and gas found in igneous rocks. This research explores the prospects, challenges and way forward in the use of hydraulic fracturing to increase the porosity of igneous rock for commercial production of oil and gas.

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Yanto, Iwan Tri Riyadi, Edi Sutoyo, Ani Apriani e Okki Verdiansyah. "Fuzzy Soft Set for Rock Igneous Clasification". In 2018 International Symposium on Advanced Intelligent Informatics (SAIN). IEEE, 2018. http://dx.doi.org/10.1109/sain.2018.8673383.

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7

M. Minarik, Michal. "IGNEOUS ROCK FROM AN AREA CALLED PODHURA". In 16th International Multidisciplinary Scientific GeoConference SGEM2016. Stef92 Technology, 2016. http://dx.doi.org/10.5593/sgem2016/b11/s01.033.

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Rodriguez, C., J. Hernandez, S. Villarroel, K. Lyons, E. Galvan e M. El-Toukhy. "Potential Igneous Intrusions Offshore Mexico: Exploration Significance". In 81st EAGE Conference and Exhibition 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201901552.

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Yanhui*, Wu, Ke Benxi, Tang Bowen e Liu Jianhong. "Multiple attenuation techniques in igneous rock area". In SPG/SEG 2016 International Geophysical Conference, Beijing, China, 20-22 April 2016. Society of Exploration Geophysicists and Society of Petroleum Geophysicists, 2016. http://dx.doi.org/10.1190/igcbeijing2016-065.

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10

Millett, J. C. F. "The shock Hugoniot of two igneous rocks". In Shock compression of condensed matter. AIP, 2000. http://dx.doi.org/10.1063/1.1303687.

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Rapporti di organizzazioni sul tema "Igneous"

1

Newberry, R. J. The Mount Fairplay igneous complex. Alaska Division of Geological & Geophysical Surveys, giugno 2020. http://dx.doi.org/10.14509/30463.

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2

Whalen, J. B., e K. L. Currie. Geology, Topsails Igneous Terrane, Newfoundland. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/126760.

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3

Frizado, J. IGBA: an international igneous rock database. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/193916.

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4

Hulbert, L. Geology of the Kilohigok Basin and subjacent Booth River igneous complex and Mara River igneous sheets. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2005. http://dx.doi.org/10.4095/220360.

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5

John McCord. Igneous Consequence Modeling for the TSPA-SR. Office of Scientific and Technical Information (OSTI), ottobre 2001. http://dx.doi.org/10.2172/790806.

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6

M. Wallace. Number of Waste Package Hit by Igneous Intrusion. Office of Scientific and Technical Information (OSTI), ottobre 2004. http://dx.doi.org/10.2172/838330.

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7

P.E. Sanchez. Number of Waste Package Hit by Igneous Intrusion. Office of Scientific and Technical Information (OSTI), giugno 2005. http://dx.doi.org/10.2172/850428.

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8

M. Cline, F. Perry, G. Valentine e E. Smistad. Potential Future Igneous Activity at Yucca Mountain, Nevada. Office of Scientific and Technical Information (OSTI), maggio 2005. http://dx.doi.org/10.2172/859068.

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9

Champion, D. C., L. Highet e J. P. Thorne. Archean alkaline and related igneous rocks of Australia. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.036.

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Champion, D. C., L. Highet e M. Buddee. Mesozoic alkaline and related igneous rocks of Australia. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.038.

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