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Artykuły w czasopismach na temat "Rocks, Sedimentary"

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Edgett, Kenneth S., and Ranjan Sarkar. "Recognition of Sedimentary Rock Occurrences in Satellite and Aerial Images of Other Worlds—Insights from Mars." Remote Sensing 13, no. 21 (October 26, 2021): 4296. http://dx.doi.org/10.3390/rs13214296.

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Sedimentary rocks provide records of past surface and subsurface processes and environments. The first step in the study of the sedimentary rock record of another world is to learn to recognize their occurrences in images from instruments aboard orbiting, flyby, or aerial platforms. For two decades, Mars has been known to have sedimentary rocks; however, planet-wide identification is incomplete. Global coverage at 0.25–6 m/pixel, and observations from the Curiosity rover in Gale crater, expand the ability to recognize Martian sedimentary rocks. No longer limited to cases that are light-toned,
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Lyu, Qiqi, Shunshe Luo, Yulong Guan, Jinhua Fu, Xiaobing Niu, Liming Xu, Shengbin Feng, and Shixiang Li. "A new method of lithologic identification and distribution characteristics of fine - grained sediments: A case study in southwest of Ordos Basin, China." Open Geosciences 11, no. 1 (February 26, 2019): 17–28. http://dx.doi.org/10.1515/geo-2019-0002.

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Abstract Lithologic identification is critical for studying fine - grained sediments, which further elucidates sedimentary environment, and formation. The oil - bearing Chang 7 Section of the Yanchang Formation in Ordos Basin contains thick dark mudstone with a wide distribution, interbedded by siltstone and fine sandstone. The lacustrine fine - grained sedimentary rocks constitute the chief source rock of the Yanchang Formation. On the grounds of fine core description, thin rock slice identification and X - ray diffraction analysis, we proposed a new method based on conventional logging data.
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Zhao, Ranlei, Xiao Xu, Wentao Ma, Cunlei Li, Qiushi Zhang, and Qingyou Yue. "Reservoir Characteristics and Controlling Factors of Sedimentary Pyroclastic Rocks in Deep-Buried Basins: A Case Study of Yingtai Fault Depression, Southern Songliao Basin." Energies 15, no. 18 (September 9, 2022): 6594. http://dx.doi.org/10.3390/en15186594.

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In this article, based on core description, thin section, scanning electron microscope (SEM), well logging and reservoir physical properties, the reservoir controlling factors of sedimentary pyroclastic rocks in deep-buried basins are assessed via the relation between reservoirs and defining factors, including lithological characteristics, sedimentary microfacies and diagenesis. In addition, the contributing factors of anomalously high-porosity and high-permeability zone are analyzed. The lithological characteristics and diagenesis of the sedimentary pyroclastic rocks are closely related to re
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DA SILVA, JOSÉ LUIZ SILVÉRIO, and EGYDIO MENEGOTTO. "Aspectos Geoquímicos de Silicificações em Rochas Sedimentares no Rio Grande do Sul, Brasil." Pesquisas em Geociências 32, no. 2 (December 31, 2005): 29. http://dx.doi.org/10.22456/1807-9806.19543.

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Some exposures of silicified sedimentary rocks and duricrusts occur in the central Depressão Periférica along the edge of the Paraná Basin in Rio Grande do Sul State, in southern part of Brazil. These silicified materials were firstly studied in the petrographic aspects by Silvério da Silva & Menegotto (2002). This paper presents geochemical results of the analysis on samples of sedimentary rocks and silica duricrusts collected in two profiles (Santa Maria and Cachoeira do Sul). The relationships between the sedimentary rocks and the duricrusts, as well their probable provenance and genesi
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LINDSTRÖM, SOFIE. "Palynology of Permian shale, clay and sandstone clasts from the Basen till in northern Vestfjella, Dronning Maud Land." Antarctic Science 17, no. 1 (February 28, 2005): 87–96. http://dx.doi.org/10.1017/s0954102005002476.

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The palynological content of randomly collected sedimentary rock clasts from the till on the south-east slope of the Basen nunatak in northern Vestfjella in western Dronning Maud Land indicate that these sedimentary rocks were derived from strata of Middle Permian age. The palynological content and preservation is similar to palynofloras described from the sedimentary rocks that crop out at the Fossilryggen nunatak to the south-east, therefore, it seems likely that the Fossilryggen area represents the source of the sedimentary rock samples in the Basen till. This is further supported by known
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Bilić, Šime, and Vesnica Garašić. "PETROLOGICAL CHARACTERISTICS OF CLASTIC SEDIMENTARY ROCKS FROM THE ST. BARBARA ORE MINE IN RUDE NEAR SAMOBOR." Rudarsko-geološko-naftni zbornik 36, no. 1 (2021): 121–35. http://dx.doi.org/10.17794/rgn.2021.1.10.

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In the scope of this research, the petrographic and geochemical analyses of clastic sedimentary rocks from the St. Barbara, copper and iron ore mine in Rude near Samobor, have been made, aiming to classify and determine the provenance and environment of formation of clastic sedimentary rocks, as well as the influence of hydrothermal fluids on their properties. Eight samples were collected in total from different locations in the mine. Six of those samples have been studied in detail. The results showed structural and geochemical variability and uneven hydrothermal alteration intensity in the s
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Pujar, Anant G., A. Sreenivasa, and Ajaykumar N. Asode. "Petrography and Provenance Study of South-Central Part of Kaladgi Basin, Belgaum, Karnataka, India." International Journal of Economic and Environmental Geology 11, no. 1 (July 7, 2020): 108–12. http://dx.doi.org/10.46660/ijeeg.vol11.iss1.2020.421.

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The area under investigation covers the south-central part of Kaladgi series comprising of sedimentary rocks, mainly quartzarenites. From the geological point of view the study area comprises southcentral part of Kaladgi basin covering around 54 km2 which encompasses rocky hills of moderate height, showing three types of facies i.e., argillaceous, arenaceous and rudaceous. Among these three, arenaceous facies is more prominent in the area. These sedimentary rocks rest unconformably over gneisses. Detailed study of the rocks exposed are done by studying the petrological aspects of the rock samp
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Pujar, Anant G., A. Sreenivasa, and Ajaykumar N. Asode. "Petrography and Provenance Study of South-Central Part of Kaladgi Basin, Belgaum, Karnataka, India." International Journal of Economic and Environmental Geology 11, no. 1 (July 7, 2020): 108–12. http://dx.doi.org/10.46660/ojs.v11i1.421.

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The area under investigation covers the south-central part of Kaladgi series comprising of sedimentary rocks, mainly quartzarenites. From the geological point of view the study area comprises southcentral part of Kaladgi basin covering around 54 km2 which encompasses rocky hills of moderate height, showing three types of facies i.e., argillaceous, arenaceous and rudaceous. Among these three, arenaceous facies is more prominent in the area. These sedimentary rocks rest unconformably over gneisses. Detailed study of the rocks exposed are done by studying the petrological aspects of the rock samp
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Hu, Zeng, Fang, Qi, Yin, Chen, Li, and Zhu. "Geochemical Study of Detrital Apatite in Sediment from the Southern Okinawa Trough: New Insights into Sediment Provenance." Minerals 9, no. 10 (October 8, 2019): 619. http://dx.doi.org/10.3390/min9100619.

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Detrital apatite is a promising accessory mineral for reliable fingerprinting of the protolith composition of detrital sediment. Here, we present the geochemical compositions of detrital apatites from four sections of a high-resolution (~140 cm/kyr) sedimentary archive from the southern Okinawa Trough (SOT) for constraining sediment source rock types and establishing changes in provenance. A series of diagrams based on the geochemical data show that apatites in Section 1 derived mainly from mafic/intermediate rocks, while apatites in the three younger sections largely originated from mafic/int
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Rasbury, E. Troy, and Jennifer M. Cole. "Directly Dating Sedimentary Rocks." Paleontological Society Papers 12 (October 2006): 77–105. http://dx.doi.org/10.1017/s1089332600001364.

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This contribution seeks to provide a summary of radiometric dating techniques that are currently applicable to Phanerozoic sedimentary deposits and therefore relevant to paleontologists. First we overview the assumptions necessary for radiometric dating and introduce isochrons and concordia diagrams as methods for calculating ages and evaluating isotope systematics. We then focus on the four most promising systems: U-Pb dating of carbonates, Re-Os dating of black shales, and U-Pb and Lu-Hf dating of phosphates. We review expected geochemical behavior of daughter and parent isotopes in the cont
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Rozprawy doktorskie na temat "Rocks, Sedimentary"

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Dodd, Matthew S. "Biosignatures in Precambrian sedimentary rocks." Thesis, University College London (University of London), 2018. http://discovery.ucl.ac.uk/10055383/.

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The overarching goal of this work was to trace the origins of organic matter as a possible biosignature for early life on Earth. This work documented the petrological, structural, isotopic, elemental and molecular properties of organic matter, in a suite of sediments ranging from the Eoarchean to the Phanerozoic. Particular attention was paid to iron formations which form a major part of the Precambrian sedimentological record. Optical and micro-Raman spectroscopy were used to document the petrological occurrences of organic matter and its associated diagenetic features. Focused ion beam and t
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Tavares, Sandra Aparecida Simionato 1969. "Fósseis do afloramento Santa Irene, cretácio superior da Bacia Bauru = inferências paleoecológicas." [s.n.], 2011. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287322.

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Orientadores: Frésia Soledad Ricardi Torres Branco, Ismar de Souza Carvalho<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-18T21:34:34Z (GMT). No. of bitstreams: 1 Tavares_SandraAparecidaSimionato_M.pdf: 8529535 bytes, checksum: 81caa7b6648edbc9a42d10c5ee967375 (MD5) Previous issue date: 2011<br>Resumo: O Afloramento Santa Irene tem sido considerado um dos mais significativos da Bacia Bauru, na Formação Adamantina, pela abundancia e boa conservação de fósseis associados ali encontrados, como dentes isolados de ar
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Malik, Qamar Mehboob. "Electrical and transport properties of sedimentary reservoir rocks." Thesis, Imperial College London, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.266398.

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Hattum, Marco Willem Alexander van. "Provenance of Cenozoic sedimentary rocks of northern Borneo." Thesis, Royal Holloway, University of London, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.423143.

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Lofts, Jeremy C. "Integrated geochemical-geophysical studies of sedimentary reservoir rocks." Thesis, University of Leicester, 1993. http://hdl.handle.net/2381/35058.

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Chernoff, Carlotta. "Origin and redistribution of metals in sedimentary rocks." Diss., The University of Arizona, 2002. http://hdl.handle.net/10150/289837.

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Integrated analysis of whole-rock and mineral geochemical data from black shale and metamorphosed black shale demonstrates the importance of sulfides as trace-element hosts and reveals the influence of depositional environment on whole-rock and mineral chemistries. Detailed analysis of Fe-sulfide contents provides evidence of considerable elemental redistribution during diagenesis and metamorphism, indicating that such sulfides plausibly serve as a source of metals and other elements to epigenetic fluids. Spatial and temporal analysis of the distribution of Phanerozoic black shale, phosphorite
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Putz-Perrier, Martin W. "Distribution and scaling of extensional strain in sedimentary rocks." Thesis, Imperial College London, 2008. http://hdl.handle.net/10044/1/1293.

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For this study, spatial and size distributions of normal faults and associated tensile fractures were directly measured in deformed sedimentary rocks in three extensional regions: Kimmeridge Bay and Kilve in the UK and the Maltese Islands. The collected data allow i) quantifcation of regional extension at different scales, ii) determination of the relative importance of large and small structures, iii) quan- tifcation of the spatial heterogeneity of brittle extension, iv) comparison of scaling laws for veins and faults belonging to the same extension event, and v) analysis of the evolution of
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Ruiz, Penã Franklin J. (Franklin José) 1962. "Elastic properties of sedimentary anisotropic rocks : (measurements and applications)." Thesis, Massachusetts Institute of Technology, 1998. http://hdl.handle.net/1721.1/58361.

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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, February 1999.<br>Includes bibliographical references (leaves 75-78).<br>In multidisciplinary studies carried out in the Budare Oil Field of the Great Oficina Oil Field, there was difficulty matching well log synthetic seismograms with 2D and 3D seismic data. In addition, the seismically determined depths of reservoir horizons are greater than the well sonic log depths. To examine this discrepancy we conducted an experimental study of dynamic elastic parameters of the rocks in the oil fie
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Dalrymple, Mark. "Sedimentological evolution of the Statfjord Formation fluvial hydrocarbon reservoirs of the northern North Sea." Thesis, University of Aberdeen, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.302647.

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The sedimentological evolution of the Statfjord Formation of the Viking Graben at the Triassic - Jurassic transition is detailed by integration of studies of mineral assemblages, isotope age data, sedimentological core analysis, palaeosol / mineralogical wireline analysis and regional correlation of subsurface wireline information, combined with theories on basin evolution in continental settings. The aim of this study is to enhance the description of, and correlation within, hydrocarbon reservoirs developed within intra-continental alluvial sediments which have been deposited in areas above t
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Andrea, Martijn. "The anisotropic elastic properties of clay-rich rocks." Thesis, Imperial College London, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243413.

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Książki na temat "Rocks, Sedimentary"

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Stokes, William Lee. Sedimentary rocks. [s.l: s.n.], 1985.

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Oxlade, Chris. Sedimentary rocks. Chicago: Heinemann Library, 2011.

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Stewart, Melissa. Sedimentary rocks. Oxford: Heinemann Library, 2003.

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Sedimentary rocks. New York: Gareth Stevens Pub., 2014.

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Oxlade, Chris. Sedimentary rocks. Chicago: Heinemann Library, 2011.

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Unearthing sedimentary rocks. New York: PowerKids Press, 2014.

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Investigating sedimentary rocks. New York: PowerKids Press, 2016.

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Sedimentary petrography. Englewood Cliffs, N.J: PTR Prentice Hall, 1993.

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Sedimentary rock. Oxford: Raintree, 2007.

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Sedimentary petrology. 2nd ed. New York: Freeman, 1992.

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Części książek na temat "Rocks, Sedimentary"

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Boggiani, Paulo César. "Sedimentary Rocks." In Encyclopedia of Earth Sciences Series, 1–3. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-12127-7_253-1.

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Fernandes, Isabel, Maarten A. T. M. Broekmans, Maria dos Anjos Ribeiro, and Ian Sims. "Sedimentary Rocks." In Petrographic Atlas: Characterisation of Aggregates Regarding Potential Reactivity to Alkalis, 43–101. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-017-7383-6_3.

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Boggiani, Paulo César. "Sedimentary Rocks." In Encyclopedia of Earth Sciences Series, 816–18. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-73568-9_253.

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McCann, Tom. "Sedimentary Rocks." In Pocket Guide Geology in the Field, 119–46. Berlin, Heidelberg: Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-63082-2_5.

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Sen, Gautam. "Sedimentary Rocks." In Petrology, 299–310. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-38800-2_14.

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Stack, Kathryn M. "Sedimentary Rocks (Mars)." In Encyclopedia of Planetary Landforms, 1–9. New York, NY: Springer New York, 2014. http://dx.doi.org/10.1007/978-1-4614-9213-9_386-1.

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Stack, Kathryn M. "Sedimentary Rocks (Mars)." In Encyclopedia of Planetary Landforms, 1900–1907. New York, NY: Springer New York, 2015. http://dx.doi.org/10.1007/978-1-4614-3134-3_386.

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Greensmith, J. T. "Sedimentary structures." In Petrology of the Sedimentary Rocks, 14–38. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-011-9640-6_3.

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Rivard, Lambert A. "Sedimentary Rocks and Duricrusts." In Geohazard-associated Geounits, 1–130. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/b93844_5.

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Okrusch, Martin, and Hartwig E. Frimmel. "Sediments and Sedimentary Rocks." In Springer Textbooks in Earth Sciences, Geography and Environment, 417–52. Berlin, Heidelberg: Springer Berlin Heidelberg, 2020. http://dx.doi.org/10.1007/978-3-662-57316-7_25.

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Streszczenia konferencji na temat "Rocks, Sedimentary"

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Takahashi, Toru, and Soichi Tanaka. "Rock physics modeling of soft sedimentary rocks." In SEG Technical Program Expanded Abstracts 2009. Society of Exploration Geophysicists, 2009. http://dx.doi.org/10.1190/1.3255249.

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Borja, Ronaldo I., Pablo F. Sanz, and David D. Pollard. "Ductile Folding of Sedimentary Rocks." In GeoCongress 2006. Reston, VA: American Society of Civil Engineers, 2006. http://dx.doi.org/10.1061/40803(187)187.

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Wang, Zhijing (Zee). "Seismic anisotropy in sedimentary rocks." In SEG Technical Program Expanded Abstracts 2001. Society of Exploration Geophysicists, 2001. http://dx.doi.org/10.1190/1.1816460.

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Jin, Guodong, Tad W. Patzek, and Dmitry B. Silin. "Physics-based Reconstruction of Sedimentary Rocks." In SPE Western Regional/AAPG Pacific Section Joint Meeting. Society of Petroleum Engineers, 2003. http://dx.doi.org/10.2118/83587-ms.

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Cohen, Morrel H. "The morphology of porous sedimentary rocks." In AIP Conference Proceedings Vol. 154. AIP, 1987. http://dx.doi.org/10.1063/1.36385.

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Labus, M., and A. Lorek. "CO2-rock Interaction on the Example of Permian Sedimentary Rocks." In 77th EAGE Conference and Exhibition 2015. Netherlands: EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201413369.

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Takahashi, Toru, and Soichi Tanaka. "Rock physics modeling of soft sedimentary and hard crystalline rocks." In SEG Technical Program Expanded Abstracts 2008. Society of Exploration Geophysicists, 2008. http://dx.doi.org/10.1190/1.3059253.

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Alomari, Esraa M., Lokendra Khatri, and Kam Ng. "Mechanical and Fracture Behavior of Sedimentary Rocks Under Uniaxial Compression." In 56th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2022. http://dx.doi.org/10.56952/arma-2022-2297.

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ABSTRACT: Energy-related characterizations can provide important information regarding mechanical behavior of rocks. A series of uniaxial compression tests were carried out on intact rock samples obtained from Wyoming, USA. The physical properties of the samples (i.e., porosity and grain size) were first examined. To investigate the fracture behavior of sedimentary rocks, a compilation of published dataset and our experimental data were employed to develop a new approach for estimating uniaxial compressive strength (UCS) based on the amount of energy released during rock deformation, which is
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Helz, George. "Interpreting Re/Mo Ratios in Sedimentary Rocks." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1020.

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Meridith, Philip G., Irina O. Bayuk, Colin Jones, and Evgeni M. Chesnokov. "Experimental and theoretical modelling of sedimentary rocks." In SEG Technical Program Expanded Abstracts 1997. Society of Exploration Geophysicists, 1997. http://dx.doi.org/10.1190/1.1886187.

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Raporty organizacyjne na temat "Rocks, Sedimentary"

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Aitken, J. D. Proterozoic Sedimentary Rocks [Chapter 4: Stratigraphy]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192359.

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Jarrett, A. J. M., D. C. Champion, S. McLennan, J. R. Anderson, J. Byass, S. Webber, and S. Gilmore. Whole-rock inorganic geochemistry of sedimentary rocks from northern Australia. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.039.

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Dumurdzanov, Nikola, Todor Serafimovski, and B. C. Burchfiel. Cenozoic Sedimentary and Volcanic Rocks of Macedonia. Geological Society of America, 2004. http://dx.doi.org/10.1130/2004-dumurdzanov-macedonia.

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Lydon, J. W. The leachability of metals from sedimentary rocks. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296329.

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Mayr, U. Cretaceous and Tertiary sedimentary and intrusive rocks. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209774.

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Schlueter, E. M. Predicting the permeability of sedimentary rocks from microstructure. Office of Scientific and Technical Information (OSTI), January 1995. http://dx.doi.org/10.2172/70737.

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Peter, J. M., and M. G. Gadd. Introduction to the volcanic- and sediment-hosted base-metal ore systems synthesis volume, with a summary of findings. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328015.

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This volume presents results of research conducted during phase 5 of the Volcanic- and Sedimentary-hosted Base Metals Ore Systems project of the Geological Survey of Canada's Targeted Geoscience Initiative (TGI) program. The papers in this volume include syntheses and primary scientific reports. We present here a synopsis of the findings during this TGI project. Research activities have addressed several mineral deposit types hosted in sedimentary rocks: polymetallic hyper-enriched black shale, sedimentary exhalative Pb-Zn, carbonate-hosted Pb-Zn (Mississippi Valley-type; MVT), and fracture-co
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Fowler, M. G., M. Obermajer, and L. D. Stasiuk. Rock-Eval/TOC data for Devonian potential source rocks, Western Canada Sedimentary Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214440.

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Thorsteinsson, R., and U. Mayr. The sedimentary rocks of Devon island, canadian arctic archipelago. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122451.

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Schlueter, Erika M. Predicting the transport properties of sedimentary rocks from microstructure. Office of Scientific and Technical Information (OSTI), January 1995. http://dx.doi.org/10.2172/79095.

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