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Books on the topic 'Amphibolis'

Author: Grafiati
Published: 4 June 2021
Last updated: 14 February 2022

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1

Amphibolie der Reflexionsbegriffe und transzendentale Reflexion: Das Amphibolie-Kapitel in Kants Kritik der reinen Vernunft. Würzburg: Königshausen & Neumann, 2012.

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2

A, Valetov T., and Vasilʹev Evgeniĭ Konstantinovich, eds. Upori͡a︡dochennostʹ kationov v amfibolakh. Moskva: "Nauka", 1986.

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3

Page, Norman J. Composition of primary postcumulus amphibole and phlogopite within an olivine cumulate in the Stillwater Complex, Montana. Washington: U.S. Geological Survey, 1987.

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4

Ivanovich, Lennykh Vladimir, and Ivanov Svi͡a︡toslav Nestorovich, eds. Amfiboly golubykh slant͡s︡ev Urala. Moskva: "Nauka", 1988.

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5

Daziano, Carlos Oscar. Las anfibolitas de la Sierra Chica de Córdoba, Argentina. [Córdoba, Argentina]: Universidad Nacional de Córdoba, 2004.

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6

Distanova, A. N. Amfiboly i biotity rannepaleozoĭskikh granitoidov Tuvy i Zabaĭkalʹi͡a︡. Novosibirsk: "Nauka," Sibirskoe otd-nie, 1990.

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7

Awdankiewicz, Honorata. Petrologia i geochemia metabazytów masywu Niedźwiedzia na bloku przedsudeckim: The petrology and geochemistry of the metabasites of the Niedźwiedź Massif in the Fore-Sudetic Block. Warszawa: Państwowy Instytut Geologiczny, 2008.

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8

Nijland, Teunis Gerrit. The Bamble amphibolite to granulite facies transitions zone, Norway. [Utrecht: Faculteit Aardwetenschappen der Rijksuniversiteit Utrecht, 1993.

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9

Virta, Robert L. The phase relationship of talc and amphiboles in a fibrous talc sample. Pittsburg, Pa: U.S. Dept. of the Interior, Bureau of Mines, 1985.

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10

Kukla, Christine. Strontium isotope heterogeneities in amphibolite facies, banded metasediments--a case study from the late Proterozoic Kuiseb Formation of the southern Damara Orogen, central Namibia. Windhoek, Namibia: Ministry of Mines and Energy, Geological Survey of Namibia, 1993.

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11

Litvin, M. A. Opticheskie spektry i okraska porodoobrazui͡u︡shchikh amfibolov. Kiev: Nauk. dumka, 1992.

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12

Gefügeuntersuchungen an Amphiboliten der Böhmischen Masse unter besonderer Berücksichtigung der Anisotropie der magnetischen Suszeptibilität. Stuttgart: E. Schweizerbart, 1995.

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13

Donato, Mary M. A newly recognized ductile shear zone in the northern Klamath Mountains, Oregon: Implications for Nevadan accretion. Washington: U.S. G.P.O., 1992.

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14

I, Slabunov A., and Rybakov Sergeĭ Ivanovich, eds. Amfibolity i rannie bazit-ulʹtrabazity dokembrii͡a︡ Severnoĭ Karelii. Leningrad: "Nauka," Leningradskoe otd-nie, 1989.

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15

Phillips, Emrys. Mineralogical and P-T studies on a series of metabasic amphibolites exposed within sheet 63E (Dalwhinnie) Scotland. [Edinburgh]: British Geological Survey, 1993.

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16

Garde, Adam A. Accretion and evolution of an Archaean high-grade grey gneiss-amphibolite complex: The Fiskefjord area, southern West Greenland. Copenhagen, Denmark: Geological Survey of Denmark and Greenland, Ministry of Environment and Energy, 1997.

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17

Bernage, Georges. Omaha Beach: 6 juin 1944. Bayeux: Heimdal, 2001.

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18

Omaha Beach: 6 June 1944. Bayeux: Heimdal, 2002.

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19

Bernage, Georges. Omaha Beach: 6 juin 1944. Bayeux: Heimdal, 2001.

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20

Veblen, David R., and Paul H. Ribbe, eds. Amphiboles. De Gruyter, 2018. http://dx.doi.org/10.1515/9781501508196.

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21

Hawthorne, Frank C., Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, eds. Amphiboles. De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523.

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22

Ernst, W. G. Amphiboles: Crystal Chemistry Phase Relations and Occurrence. Springer, 2012.

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23

The Battle for Amphibopolis. Graphix, 2017.

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24

C, Hawthorne Frank, Mineralogical Society of America, and Accademia nazionale dei Lincei, eds. Amphiboles: Crystal chemistry, occurrence, and health issues. Chantilly, Va: Mineralogical Society of America, 2007.

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25

AMPHIBOLES: Crystal Chemistry, Occurrence, and Health Issues, Rimg. Mineralogical Society of Amer, 2007.

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26

Tipomorfizm amfibolov iz metabazitov Ukrainskogo shchita. Kiev: Nauk. dumka, 1991.

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27

TenNapel, Doug. The Battle for Amphibopolis (Nnewts #3). Graphix, 2017.

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28

Lauf, R. J. Collector's guide to the amphibole group. 2015.

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29

The King of Amphiboly: A Fable. Vantage Press, 2007.

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30

Hilyard, Mark D. Partitioning of rare earth and high field strength elements between pargasitic amphibole and silicate melts. 1997.

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31

Burr, George S. Assimilation of amphibolite by andesite magma: Physical-chemical effects and petrologic implications. 1993.

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32

Vaughan, David. 1. The mineral world. Oxford University Press, 2014. http://dx.doi.org/10.1093/actrade/9780199682843.003.0001.

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Minerals are the fundamental components of the Earth. ‘The mineral world’ describes the fields of mineralogy and crystallography that study them. There are approximately 4,400 known minerals, but the ‘big ten’ minerals that are most abundant in the rocks of the Earth’s crust and Upper Mantle are calcite, quartz, olivines, pyroxenes, amphiboles, muscovite, biotite, orthoclase, albite, and anorthite. The two essential characteristics of any mineral are its chemical composition and its crystal structure. Minerals can be assigned to one of seven crystal classes depending on their elements of symmetry. There is further subdivision into 32 crystal classes. Minerals are classified by chemical composition into mineral groups such as silicates, and carbonates.
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33

Laurs, Brendan M. Emerald mineralization and amphibolite wall-rock alteration at the Khaltaro pegmatite-hydrothermal vein system, Haramosh Mountains, Northern Pakistan. 1995.

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34

W, Tabor R., and Geological Survey (U.S.), eds. Major-and trace-element composition of greenstones, greenschists, amphibolites, and selected mica schists and genisses from the North Cascades, Washington. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1985.

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35

Major-and trace-element composition of greenstones, greenschists, amphibolites, and selected mica schists and genisses from the North Cascades, Washington. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1985.

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36

Major-and trace-element composition of greenstones, greenschists, amphibolites, and selected mica schists and genisses from the North Cascades, Washington. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1985.

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37

Major-and trace-element composition of greenstones, greenschists, amphibolites, and selected mica schists and genisses from the North Cascades, Washington. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1985.

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38

W, Tabor R., and Geological Survey (U.S.), eds. Major-and trace-element composition of greenstones, greenschists, amphibolites, and selected mica schists and genisses from the North Cascades, Washington. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1985.

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39

Bernage, Georges. Omaha Beach: 6/6/1944. Heimdal, 2002.

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40

1952-, Burton William C., and Geological Survey (U.S.), eds. 40Ar/39 Ar age-spectrum data for amphibole, muscovite, biotite, and K-feldspar samples from metamorphic rocks in the Blue Ridge anticlinorium, northern Virginia. [Denver, CO]: U.S. Geological Survey, 1999.

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41

1952-, Burton William C., and Geological Survey (U.S.), eds. 40Ar/39 Ar age-spectrum data for amphibole, muscovite, biotite, and K-feldspar samples from metamorphic rocks in the Blue Ridge anticlinorium, northern Virginia. [Denver, CO]: U.S. Geological Survey, 1999.

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42

1952-, Burton William C., and Geological Survey (U.S.), eds. 40Ar/39 Ar age-spectrum data for amphibole, muscovite, biotite, and K-feldspar samples from metamorphic rocks in the Blue Ridge anticlinorium, northern Virginia. [Denver, CO]: U.S. Geological Survey, 1999.

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43

1952-, Burton William C., and Geological Survey (U.S.), eds. 40Ar/39 Ar age-spectrum data for amphibole, muscovite, biotite, and K-feldspar samples from metamorphic rocks in the Blue Ridge anticlinorium, northern Virginia. [Denver, CO]: U.S. Geological Survey, 1999.

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44

1952-, Burton William C., and Geological Survey (U.S.), eds. 40Ar/39 Ar age-spectrum data for amphibole, muscovite, biotite, and K-feldspar samples from metamorphic rocks in the Blue Ridge anticlinorium, northern Virginia. [Denver, CO]: U.S. Geological Survey, 1999.

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45

Fischer, Jeffrey Charles. Field and geochemical study of amphibolites and basic dikes of the Hyde School and Fish Creek bodies of the Hyde School Gneiss, Adirondack Lowlands, New York. 1995.

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46

1952-, Burton William C., and Geological Survey (U.S.), eds. p40sAr/p39sAr age-spectrum data for amphibole, muscovite, biotite, and K-feldspar samples from metamorphic rocks in the Blue Ridge anticlinorium, northern Virginia. [Denver, CO]: U.S. Geological Survey, 1999.

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47

Bridges, John C. Evolution of the Martian Crust. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190647926.013.18.

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This is an advance summary of a forthcoming article in the Oxford Encyclopedia of Planetary Science. Please check back later for the full article.Mars, which has a tenth of the mass of Earth, has cooled as a single lithospheric plate. Current topography gravity maps and magnetic maps do not show signs of the plate tectonics processes that have shaped the Earth’s surface. Instead, Mars has been shaped by the effects of meteorite bombardment, igneous activity, and sedimentary—including aqueous—processes. Mars also contains enormous igneous centers—Tharsis and Elysium, with other shield volcanoes in the ancient highlands. In fact, the planet has been volcanically active for nearly all of its 4.5 Gyr history, and crater counts in the Northern Lowlands suggest that may have extended to within the last tens of millions of years. Our knowledge of the composition of the igneous rocks on Mars is informed by over 100 Martian meteorites and the results from landers and orbiters. These show dominantly tholeiitic basaltic compositions derived by melting of a relatively K, Fe-rich mantle compared to that of the Earth. However, recent meteorite and lander results reveal considerable diversity, including more silica-rich and alkaline igneous activity. These show the importance of a range of processes including crystal fractionation, partial melting, and possibly mantle metasomatism and crustal contamination of magmas. The figures and plots of compositional data from meteorites and landers show the range of compositions with comparisons to other planetary basalts (Earth, Moon, Venus). A notable feature of Martian igneous rocks is the apparent absence of amphibole. This is one of the clues that the Martian mantle had a very low water content when compared to that of Earth.The Martian crust, however, has undergone hydrothermal alteration, with impact as an important heat source. This is shown by SNC analyses of secondary minerals and Near Infra-Red analyses from orbit. The associated water may be endogenous.Our view of the Martian crust has changed since Viking landers touched down on the planet in 1976: from one almost entirely dominated by basaltic flows to one where much of the ancient highlands, particularly in ancient craters, is covered by km deep sedimentary deposits that record changing environmental conditions from ancient to recent Mars. The composition of these sediments—including, notably, the MSL Curiosity Rover results—reveal an ancient Mars where physical weathering of basaltic and fractionated igneous source material has dominated over extensive chemical weathering.
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48

E&G – Quaternary Science Journal Vol. 58 No 2: CHANGING ENVIRONMENTS – YESTERDAY, TODAY, TOMORROW. Geozon Science Media, 2010.

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