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TYPES OF METAMORPHISM AND METAMORPHIC ROCKS
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Recall that three conditions cause metamorphism: rising temperature, rising pressure, and changing chemical environment. In addition, tectonic deformation develops foliation and thus strongly affects the texture of a metamorphic rock. These conditions occur in four geologic environments.
Contact metamorphism occurs where hot magma intrudes cooler country rock. The country rock may be of any type – sedimentary, metamorphic, or igneous. The highest-grade metamorphic rocks form at the contact, closest to the magma. Lower-grade rocks develop farther out. A metamorphic halo around a pluton can range in width from less than a meter to hundreds of meters, depending on the size and temperature of the intrusion and the effects of water or other fluids.
Contact metamorphism commonly occurs without deformation. As a result, the metamorphic minerals grow with random orientations, and the rocks develop no metamorphic layering.
Common Contact Metamorphic Rocks
The hornfels is a hard, dark, fine-grained rock usually formed by contact metamorphism of shale. Mica and chlorite are common in the cooler, outer parts of a hornfels halo. Hornblende and other amphiboles occur in the middle of the halo, and pyroxenes can form next to the pluton, in the highest-temperature zone. Quartz and feldspar are common throughout the halo, because they are stable over a wide temperature range.
Burial metamorphism results from deep burial of rocks in a sedimentary basin. A large river carries massive amounts of sediment to the ocean every year, where it accumulates on a delta. Over tens or even hundreds of millions of years, the weight of the sediment becomes so great that the entire region sinks isostatically. Younger sediment may bury the oldest layers to a depth of more that 10 kilometers in a late basin. Because rocks are heavy, pressure within the Earth increases rapidly with depth. Over time, temperature and pressure increase within the deeper layers until burial metamorphism begins.
Burial metamorphism occurs without tectonic deformation. Consequently, metamorphic minerals grow with random orientations, and, like contact metamorphic rocks, burial metamorphic rocks are unfoliated.
Common Burial Metamorphic Rocks
Because of the lack of deformation, rocks formed by burial metamorphism often retain sedimentary structures. Shales and siltstones become harder and better lithified to form argillitewhich looks like the parent rock although new minerals have replaced the original ones. Quartz sandstone becomes quartzite. When sandstone is broken, the fractures occur in the cement between the sand grains. In contrast, quartzite becomes so firmly cemented during metamorphism that the rock fractures through the grains. Burial metamorphism converts limestone and dolomite to marble.
Regional metamorphism occurs in and near a subduction zone, where tectonic forces build mountains and deform rocks. It is the most common and wide-spread type of metamorphism and affects broad regions of the Earth’s crust.
Magma forms in a subduction zone, where oceanic lithosphere is sinking beneath a continent. As the magma rises, it heats large regions of the crust. The high temperatures cause new metamorphic minerals to form throughout the region. At the same time, the tectonic forces squeeze and deform rock. The rising magma further deforms the hot, plastic country rock as it forces its way upward. As a result of all of these processes acting together, regionally metamorphosed rocks are strongly foliated and are typically associated with mountains and igneous rocks. Regional metamorphism produces zones of foliated metamorphic rock tens to hundreds of kilometers across.
Common Rocks Formed by Regional Metamorphism
Shale consists of clay minerals, quartz, and feldspar and is the most abundant sedimentary rock. Shale undergoes a sequence of changes as metamorphic grade increases.
At definite temperatures certain metamorphic minerals are stable. Thus, it shows the sequence in which minerals appear, and then decompose, as metamorphic grade increases. As regional metamorphism begins, the clay minerals break down and are replaced by mice and chlorite. These new, platy minerals grow perpendicular to the direction of tectonic squeezing. As a result, the rock develops slaty cleavage and is called slate (аспидный сланец). With rising temperature and continued deformation, the micas and chlorite grow larger, and wavy or wrinkled surfaces replace the flat, slaty cleavage, giving phyllite a silky appearance.
As temperature continues to rise, the mica and chlorite grow large enough to be seen by the naked eye, and foliation becomes very well developed. Rock of this type is called schist (кристаллический сланец). Schist forms approximately at the transition from low to intermediate metamorphic grades.
At high metamorphic grades, light- and dark-colored minerals often separate into bands that are thicker than the layers of schist to form a rock called gneiss (pronounced “nice”). At the highest metamorphic grade, the rock begins to melts, forming small veins of granitic magma. When metamorphism wanes and the rock cools, the magma veins solidify to form migmatite, a mixture of igneous and metamorphic rock.
Under conditions of regional metamorphism, quartz sandstone and limestone transform to foliated quartzite and foliated marble, respectively.
Water is a chemically active fluid; it attacks and dissolves many minerals. If the water is hot, it attacks minerals even more rapidly. Hydrothermal metamorphism (also called hydrothermal alteration and metasomatism) occurs when hot water and ions dissolved in the hot water react with a cork to change its chemical composition and minerals. In some hydrothermal environments, water reacts with sulfur minerals to form sulfuric acid, making the solution even more corrosive.
The water responsible for hydrothermal metamorphism can originate from three sources. Magmatic water is given off by a cooling magma. Metamorphic water is released from rocks during metamorphism. Most hydrothermal alteration, however, is caused by circulating ground water – the water that saturates soil and bedrock. Cold ground water sinks through bedrock fractures to depths of a few kilometers, where it is heated by the hotter rocks at depth or, in some cases, by a hot, shallow pluton. Upon heating, the water expands and rises back toward the surface through other fractures. As it rises, it alters the country rock through which it flows.
Rocks Formed by Hydrothermal Metamorphism
Hydrothermal metamorphism is like an accelerated from of weathering. As in weathering, feldspars and many other minerals of the parent rock dissolve. The hot water carries away soluble components, such as potassium, sodium, calcium, and magnesium. Aluminum and silicon remain because they have low solubilities. They combine with oxygen and water to from clay minerals. Hydrothermally metamorphosed rocks often have a white, bleached appearance and a soft consistence because the clays are white and soft.
Most rocks and magma contain low concentrations of metal such as copper, gold, lead, zinc, and silver. Although metals are present in very low concentrations, hydrothermal solutions sweep slowly through vast volumes of country rock, dissolving and accumulating the metals as they go. The solutions then deposit the dissolved metals when they encounter changes in temperature, pressure, or chemical environment. In this way, hydrothermal solutions scavenge and concentrate metals from average crustal rocks and then deposit them locally to form ore.
1. What three conditions cause metamorphism?
2. When does contact metamorphism occur?
3. What does burial metamorphism result from?
4. Where does regional metamorphism occur?
5. What is hydrothermal metamorphism?
6. Where does the water responsible for hydrothermal alteration originate?
a) State to what part of speech the words belong and from what words they are formed. Translate them into Russian:
deformation; recombine; indirectly; difference; effectiveness; redeposition; invariably; uselessness; width; countless; replace; decompose; resolidified; harden; disappearance; instability; irregularity.
b) Fill in the blanks with the adjectives formed from underlined verbs or nouns:
1. Under the action of pressure and high temperature rocks change their composition and structure. One may say that the structure and composition of rocks are . . . .
2. Everybody understands that metamorphic rocks have been developed from earlier igneous and sedimentary rocks. It is quite . . . . that these changes take place in texture, in mineral composition and in structural features of rocks.
3. Soft rocks can break into pieces. They are . . . .
4. Rare metals are of great value. They are very . . . .
5. Rock pressure and temperature vary. The role of water in metamorphism is determined by four . . . . parameters.
a) Find in the right column Russian equivalents of the following words and word combinations:
1) The highest grade metamorphic rocks 1) Кливаж сланцеватости
2) Contact metamorphism 2) Высокосортные метаморфичес-
3) Hornfels кие породы
4) Gneiss 3) насыщать почву и коренную
5) Burial metamorphism породу
6) Slaty cleavage 4) (Кристаллический) сланец
7) Schist 5) Роговик
8) To saturate soil and bedrock 6) Гнейс
9) Hornblende 7) Амфибол, роговая обманка
10) Foliated metamorphic rocks 8) Метаморфизм захоронения
9) Слоистые метаморфические
10) Контактный метаморфизм
b) Translate into English using the following words and word combinations:
1. Контактный метаморфизм происходит там, где горячая магма внедряется в более холодную коренную породу.
2. Роговик – это тяжелая, темная, мелкозернистая порода, сформированная обычно контактным метаморфизмом глинистого сланца.
3. Метаморфизм захоронения является результатом глубокого захоронения пород в бассейне осадконакопления.
4. Региональный метаморфизм происходит в зоне субдукции или около нее, где тектонические силы создают (строят) горы и нарушаю (деформируют) породу.
5. Гидротермальный метаморфизм происходит, когда горячая вода и ионы, растворенные в горячей воде, вступают в реакцию с породой, изменяя ее химический состав и минералы.
Metamorphism is the process by which solid rocks and minerals change in response to changing environmental conditions.
Most metamorphic reactions occur because each mineral is stable only within a certain range of temperature, pressure, and chemical environment.
Both the texture and the minerals can change as a rock is metamorphosed.
Contact metamorphism occurs when an igneous intrusion heats nearby country rock. Burial metamorphism results from increasing temperature and pressure caused by burial or rocks, commonly within a sinking sedimentary basin. Both types of metamorphism produce nonfoliated metamorphic rocks. Regional metamorphism forms foliatedrocks. Hydrothermal metamorphism occurs when hot, migrating fluids change the chemical composition of country rock.
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