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Редактор(ы):Hesselbo S.P., Parkinson D.N.
Издание:The Geological Society of London, 1996 г., 276 стр., ISBN: 1-897799-49-7
Язык(и)Английский
Sequence stratigraphy in British geology / Секвенс-стратиграфия в геологии Британии

Hesselbo, S. P. & Parkinson, D. N. Sequence stratigraphy in British Geology Non-marine and paralic sequences
Burgess, P. M. & Allen, P. A. A forward-modelling analysis of the controls on sequence stratigraphical geometries
Leeder, M. R. & Stewart, M. D. Fluvial incision and sequence stratigraphy: alluvial responses to relative sea-level fall and their detection in the geological record
Wonham, J. P. & Elliot, T. High-resolution sequence stratigraphy of a mid-Cretaceous estuarine complex: the Woburn Sands of the Leighton Buzzard area, southern England
Wright, V. P. The use of palaeosols in sequence stratigraphy of peritidal carbonates
Shallow marine sequences

Редактор(ы):Felt V.L., Johannessen E.P., Mathieu, Steel R.J.
Издание:Elsevier, 1995 г., 588 стр., ISBN: 0-444-81863-4
Язык(и)Английский
Sequence stratigraphy on the Northwest European margin / Секвенс-стратиграфия северо-западной Европы

Significant problems are being encountered by stratigraphers as they attempt to apply Exxonian sequence analysis to the depositional record. The most serious problem is one of consistent and objective boundary recognition. The unconformable portion of the boundary usually can be recognized with reasonable objectivity but a major problem occurs when the boundary is a "correlative conformity". The Exxon model defines such a surface as the depositional surface which existed at the time of the end of base level (relative sea level) fall. In many cases this theoretical surface has no apparent lithologic expression and cannot be recognized objectively. Thus correlation of a depositional sequence throughout a basin is either impossible or is an extremely subjective exercise.

Автор(ы):Speight J.G.
Издание:Elsevier, 2012 г., 192 стр., ISBN: 9780124017214
Язык(и)Английский
Shale Oil Production Processes / Добыча сланцевой нефти

Shale Oil represents a huge additional global fossil fuel resource. However, extracting oil from the shale is no simple task; much still needs to be understood to make the process more cost-effective to increase economic flow rates. Clear and rigorous, Oil Shale Production Process will prove useful for those scientists and engineers already engaged in fossil fuel science and technology as well as scientists, non-scientists, engineers, and non-engineers who wish to gain a general overview or update of the science and technology of fossil fuels. Not only does the book discuss the production processes but also provides methods which should reduce environmental footprint by properly addressing: surface mining and extraction processes, in situ conversion process and hydrotreatment.

Редактор(ы):Dewers T., Heath J., Sanchez M.
Издание:Wiley, 2020 г., 299 стр., ISBN: 9781119066682
Язык(и)Английский
Shale. Subsurface science and engineering / Сланец. Наука и техника о недрах

Part I: Shale and Clay Overview

1. Mudrock Components and the Genesis of Bulk Rock Properties: Review of Current Advances and Challenges Kitty L. Milliken and Nicholas W.Hayman

2. Chemical Composition of Formation Water in Shale and Tight Reservoirs: A Basin‐Scale Perspective Yousif Kharaka, Kathleen Gans, Elisabeth Rowan, James Thordsen, Christopher Conaway, Madalyn Blondes, and Mark Engle

3. From Nanofluidics to Basin‐Scale Flow in Shale: Tracer Investigations Yifeng Wang

4. Metals in Oil and Gas‐Bearing Shales: Are They Potential (Future) Ore Deposits? Mark J. Rigali and James L. Krumhansl

Издание:DGGV, 2012 г., 308 стр., ISBN: 978-3-433-03140-7
Язык(и)Английский
Shallow geothermal systems – Recommendations on design, construction, operation and monitoring / Неглубокие геотермальные системы – Рекомендации по проектированию, строительству, эксплуатации и мониторингу

The use of shallow geothermal energy has increased enormously over the past ten years. As the number of geothermal energy installations has risen, so has the number of technical developments in the field. There have been cases of damage in connection with the construction and operation of geothermal energy systems which have attracted much attention in the media. In particular, the cases of damage that have become public show that drilling to depths of several hundred metres is a technical activity that calls for responsible procedures in the sense of quality-assured design, construction and operation of the systems. Avoiding damage caused by shallow geothermal energy installations is a top priority for sustainable geothermal energy uses, especially when bodies of groundwater have to be protected against adverse effects.

Редактор(ы):Dillon P., Simmers I.
Издание:A.A.Balkema, 1998 г., 240 стр., ISBN: 90-8410-442-2
Язык(и)Английский
Shallow groundwater systems / Неглубокие системы подземных вод

Unsaturated-saturated zone processes

Vertical heterogeneity in soil properties and contaminant transport through soil profiles 

Kookana, R.S. & Naidu, R.

Solute transport in the surface soil

Snow, V.O., Clothier, B.E. & Tillman, R. W.

Laboratory and field application of a twin disk infiltrometer for measurement of soil hydraulic properties

Smettem, K.R.J., Ross, P.J., Haverkamp, R., Parlange, J.Y., & Gregory, P.J.

Seasonal dynamics of stream networks in shallow groundwater systems: A simple analytical approach 

De Vries, J.J.

Автор(ы):Goldring R.
Издание:Geological society of London, 1971 г., 99 стр.
Язык(и)Английский
Shallow-water sedimentation as illustrated in the upper devonian baggy beds / Мелководное осадкообразование на примере верхнедевонских впадин

The baggy beds of north devon and west Somerset comprise some 440 m of shallow-water marine sandstones and shales of Upper Devonian (Famennian) age. They succeed the Pickwell Down Sandstone and Upcott Beds of Old Red Sandstone facies, and are followed by the Pilton Beds, a neritic facies. The lower part of the Pilton Beds has been correlated with the Wocklumeria Stage (Stufe) VI of the Famennian (Goldring 1955, 1957). Unpublished work on the conodont and spore assemblages indicates that the Baggy Beds are also of Wocklumeria age (R. Austin, G. Dolby & J. Williams, personal communication).  <...>

Выпуск 50
Автор(ы):Austrheim H., Griffin W.L.
Издание:Journal Chemical Geology, Amsterdam, 1985 г., 15 стр.
Язык(и)Английский
Shear deformation and eclogite formation within granulite-facies anorthosites of the bergen arcs, Western Norway

Austrheim, H. and Griffin, W.L., 1985. Shear deformation and eclogite formation within granulite-facies anorthosites of the Bergen Arcs, western Norway. In: D.C. Smith, G. Franz and D. Gebauer (Guest-Editors), Chemistry and Petrology of Eciogites. Chem. Geol., 50: 267—281.

The anorthosites of the Bergen Arcs contain two distinct metamorphic mineral assemblages which are stable under different P—T conditions. A granulite-facies assemblage, which equilibrated at T = 800—900° C, P < 10 kbar, is defined by the minerals plagioclase, Al-rich diopside (Cpx I), garnet (Gnt I) ± scapolite ± orthopyroxene + dark-brown hornblende. This assemblage is linked by corona structures to a primary mag-matic mineralogy, where coexistence of olivine and plagioclase limits the maximum crystallization pressure of the anorthosites to ~ 8 kbar at 1200°C. The anorthosites are transected by a series of fine-grained shear zones in which the granulite-facies assemblage is replaced by an eclogite mineralogy defined by omphacite (Cpx II) (Jd40_i0) + garnet + kyanite + epidote/clinozoisite + phengite + quartz ± amphibole with plagioclase sometimes remaining in the marginal parts. Mineral compositions indicate equilibration conditions for the eclogite paragenesis of Г = 700—800° С, Р = 16—19 kbar.

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