Редактор(ы):Rubie D.C., Thompson A.B.
Издание:Springer-Verlag, 1985 г., 300 стр., ISBN: 978-1-4612-9548-8
Advances in physical geochemistry. Volume 4. Metamorphic reactions. Kinetics, textures and deformation / Успехи физической геохимии. Выпуск 4. Метаморфические реакции. Кинетика, текстуры и деформация

It is very common to find that in mineral synthesis experiments the crystals that form first have disordered cations, even when the synthesis conditions are well within the stability field of the ordered state. Some examples are the crystallization of albite from glass starting material (MacKenzie, 1957) or a flux (Woensdregt, 1983), cordierite from glass (Schreyer and Schairer, 1961; Putnis, 1980a), and plagioclase from glass (Eberhard, 1967; Kroll and Muller, 1980).

Издание 5
Автор(ы):Winkler H.G.F.
Издание:Springer Science+Business Media B.V., 1979 г., 358 стр., ISBN: 978-0-387-90413-9
Petrogenesis of Metamorphic Rocks / Петрогенезис (петрология) метаморфических горных пород

Igneous rocks formed at relatively high temperatures of approximately 650° to 1200°C and sediments deposited at the earth's surface represent extreme ends of the temperature range realized in the processes of rock formation.

Автор(ы):Spry A.
Издание:Pergamon, 1969 г., 384 стр.
Metamorphic textures / Метаморфические текстуры

METAMORPHISM is the mineralogical and structural (textural) adjustment of (dominantly) solid rocks to physical and chemical conditions which differ from those under which the rocks originated. Weathering and similar processes are conventionally excluded. The type of metamorphism depends on the relative values of temperature ( T ) , confining pressure (/*con)> pressure or chemical activity or fugacity of water (expressed generally as PHJO)* deformation or directed pressures (P^ir) and their variation with time {t). There is only a limited degree of interdependence of these controls and the metamorphic history of a rock is an expression of their mutual interaction with time (Fyfe, Turner and Verhoogen, 1958; Pitcher and Flinn, 1965). <...>

Автор(ы):Bruce W.D.Yardley, Guilford C., MacKenzie W.S.
Издание:Longman, 1990 г., 125 стр., ISBN: 0-470-21677-8
Atlas of metamorphic rocks and their textures / Атлас метаморфических пород и их текстур

The study of rocks in thin section using a petrographic microscope is an essential part of any undergraduate course in geology. This is the fourth volume in a series of photographic atlases of minerals and rocks in thin section. As in previous volumes the main purpose of the book is to provide the student with a handbook for use in practical classes to enable him or her to become familiar with the more common mineral associations and textures to be found in metamorphic rocks. In addition, some more unusual rocks which have given rise to particular significant ideas about metamorphism are also illustrated; the aim of this atlas is however to complement, not replace, a theoretical course in metamorphism.

Издание 7
Автор(ы):Bucher K., Frey M.
Издание:Springer Science+Business Media B.V., 2002 г., 349 стр., ISBN: 978-3-662-04916-7
Petrogenesis of Metamorphic Rocks / Петрогенезис (петрология) метаморфических горных пород

The process of rock metamorphism changes the mineralogical and chemical composition, as well as the structure of rocks. Metamorphism is typically associated with elevated temperature and pressure; thus it affects rocks within the earth's crust and mantle. The process is driven by changing physical and or chemical conditions in response to large-scale geological dynamics.

Автор(ы):Kornprobst J.
Издание:Kluwer Academic Publishers, 2002 г., 224 стр., ISBN: 0-306-48097-2
Petrology and structural geology. Volume 12. Metamorphic rocks and their geodynamic significance. A petrological handbook / Петрология и структурная геология. Выпуск 12. Метаморфические породы и их геодинамическое значение. Петрологический справочник

Metamorphism is the sum of all transformations which cause a rearrangement of the elements of a rock at the atomic scale, leading to a recrystallization in the solid state (with or without a fluid phase), as a result of variations in temperature, pressure or of composition.

ТематикаГеодинамика, Петрография
Издание 2
Автор(ы):Mason R.
Издание:Springer Science+Business Media B.V., 1990 г., 240 стр., ISBN: 978-94-017-2590-3
Petrology of the metamorphic rocks / Петрология метаморфических пород

There are three categories of rocks- igneous, sedimentary and metamorphic. Igneous rocks have been formed by solidification of hot silicate melts known as magmas, which may be erupted at the Earth's surface as lavas from volcanoes. Sedimentary rocks form by a variety of processes at low temperatures near the surface, including the bottom of the seas and oceans. Metamorphic rocks, the third category, were originally either igneous or sedimentary, but their character has been changed by processes operating below the surface of the Earth. The constituent minerals of the rocks may be changed, or the shapes, sizes and mutual spatial relationships of the crystals may change. There are a variety of processes involved, and they are collectively described by the term metamorphism. <...>

Автор(ы):Галдин Н.Е.
Редактор(ы):Резанов И.А.
Издание:Недра, Москва, 1977 г., 127 стр., УДК: 551.14/16:53
Физические свойства глубинных метаморфических и магматических пород при высоких давлениях и температуре

Описаны физико-механические свойства горных пород (скорость распространения упругих воли, плотность, пористость, анизотропность и др.). детально изученные при давлении до 20 кбар и температуре до 300°С. Измерения производились на образцах глубинных магматических и метаморфических пород амфиболитовой, гран\лнтовой и эклогитовой фации метаморфизма, отобранных систематически по отдельным блокам и комплексам восточной части Балтийского щита. Изучены коллекции образцов пород с Анабарского массива, из трубок взрыва на Сибирской платформе И на Памире, из глубоких скважин на Русской платформе. Детально изучались петрохимические, петрографические и структурные особенности пород.

Автор(ы):Сомин М.Л.
Редактор(ы):Белоусов В.В.
Издание:Наука, Москва, 1971 г., 255 стр., УДК: 551
Доюрское основание главного хребта и южного склона Большого Кавказа

Работа посвящена основным проблемам геологии доальпийского основания зон Главного хребта и южного склона Большого Кавказа. Рассматриваются стратиграфия, вещественный состав, история метаморфизма и тектоническая структура комплексов пород доюрского возраста. Особое внимание уделено вопросам возраста метаморфических толщ  Главного хребта, роли изоклинальной складчатости в их структу-
ре, структурной зональности, а также стратиграфия доюрского комплекса Сванетского антиклинория и проблеме «сквозного» развитии геосинклинали южного склона. Рассматриваются роль альпийских движений в формировании структуры доюрского основания, положение в нем грани-тоидов и общие особенности развития Большого Кавказа на доальпий-ских этапах

Редактор(ы):Bayly M.B., Borradaile G.J., Powell C.McA.
Издание:Springer-Verlag, 1982 г., 546 стр., ISBN: 978-3-642-68434-0
Atlas of deformational and metamorphic rock fabrics / Атлас деформационно-метаморфических структур горных пород

Our knowledge of metamorphic and deformational rock fabrics has been acquired largely by studying the products of deformation in ancient fold belts. As such, our understanding of how rock fabrics form has been built up from inferences about, rather than direct observations of, processes that might have operated, and many of those inferences have proved incorrect.

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