 | | Journal (article/letter/editorial) | | 102-109, 1981. GARNET-CLINOPYROXENE KUROSEGAWA AMPHIBOLITE TECTONIC ZONE, CITY-PETROGRAPHY FROM NEAR...surrounded clinopyroxene-bearing partly by amphibolite serpentinite of the mass Kurosegawa 0.2 x 1.1...indicates that partitioning the coefficient amphibolite was between coexisting formed under the...surrounding Chichibu System are always accompanied by serpentinite. Zone have been 1) biotite-bearing•@ 2)...augite-garnet garnet amphibolite (Karakida, 1977), amphibolite, garnet amphibolite and garnet-clinopyroxene |  | | Book | | MOLDAN UBIAN s. str. Gfohl unit < Ci MORAVO - SILESIAN (medium to high grade) D Drosendorf unit (low...Evolution S. VRANA, P. BLUMEL, and K. VIII Moravo-Silesian Zone VIII. A Introduction Z. MfsAR and M. X...Igneous Activity (Cadomian Plutonism in the Moravo-Silesian Basement) F. FINGER, G. FRASL, A. DUDEK, E. JELiNEK...and Metallurgy AI. Mickiewicza 30 30059 Krakow Poland P. BLilMEL Institut fur Mineralogie Technische...Geological Sciences Cybulskiego 30 50205 Wroclaw Poland E. JELINEK Department of Geology Charles University |  | | Journal (article/letter/editorial) | | metamorphosed Precambrian and Lower Paleozoic rocks in the east and lower crustal rocks in the west (Peřestý...Holub (a) SAXOTHURINGIAN / W. SUDETES / LUGIAN Lower Carboniferous clastics Proterozoic to Early Paleozoic...tur Su on ne e zo Cretaceous Basin Praha SILESIAN LUGIAN Kutná Hora Complex 50° Monotonous and... ult TEPLÁ–BARRANDIAN BRUNOVISTULIAN Moravo-Silesian (Proterozoic and Paleozoic) PC CB Ba Carboniferous...Neoproterozoic granitoids 14° (b) VP46 N MLC Amphibolite Serpentinite Toužim Ky/Sil bearing gneiss Eclogite |  | | Book | | . . . . . . . . . . . . . . . 2.3.2 Tidding Serpentinite . . . . . . . . . . . . . . . . . . . . . ....Peridotite . . . . . . . . . . . . . . . . 3.4.3 Serpentinite . . . . . . . . . . . . . . . . . . . 3.4.4...2.1 Spinel Peridotite . . . . . . . . . 5.3 Serpentinite . . . . . . . . . . . . . . . . . . 5.4 Rodingite.... . . . . . . . . . 99 99 100 101 101 10 Serpentinite . . . . . . . . . . . . . . . . . . . . . ....been achieved only down to the top of the oceanic lower crust (*1.5 km), a correlation between the Semail |  | | Journal (article/letter/editorial) | | peridotitesand amphibolitesof the Paleozoic komatiitic lower ultramafic unit, the Tjakastad Finero Complexin...slenderneedles of amphiboles,oligoclase,chlorite, zoisite,epidote, secondarycarbonate,and quartz. Opaque...volcanicassemblages at the baseof the greenstone sequencewith the lower ultramafic and the mafic to amounts of accessoryopaque...the belt in Zimbabwewas kindly (1979) named the lower unit containingultramafic Belingwegreenstone and...morphismleadingto a completeserpentinization of lower greenstones the ultramafic rocks. No olivine relicts |  | Yui, T. F., Okamoto, K., Usuki, T., Lan, C. Y., Chu, H. T., Liou, J. G. (2009) Late Triassic–Late Cretaceous accretion/subduction in the Taiwan region along the eastern margin of South China – evidence from zircon SHRIMP dating. International Geology Review, 51 (4) 304-328 doi:10.1080/00206810802636369 | Journal (article/letter/editorial) | | Metamorphosed ophiolitic rocks, such as amphibolite, metagabbro and serpentinite, occur as exotic blocks within...ferromanganoan sediments (Jahn et al. 1981), and omphacite-zoisite-albitephlogopite-quartz metabasite recorded high-pressure...gneiss, meta-andesite/granite, metabasite, amphibolite, serpentinite, marble, and metachert. All rocks have...have been subjected to greenschist- to amphibolite-facies metamorphism. Metabasites have geochemical characteristics...Garnet-chloritoid rock Marble Age (Ma) Method (mineral) Amphibolite 66–95 K–Ar (amphibole, whole rock) Tailuko |  | | Report (issue) | | Jabal al Qub............................ 24 Amphibolite..................... 6 Overview...............14 14 Ultramafic rocks.................... Amphibolite......................... Metadiorite...........the western Afif terrane...................... Amphibolite of the western Afif terrane....................the average compositions of primary spinel in serpentinite samples from the Nabitah fault zone...........Identified by a locus of northtrending, fault-bounded serpentinite bodies, the Nabitah fault system can be traced |  | | Book | | Field of the Fore-Sudetic Monocline (Southwestern Poland) S. Speczik (with 6 Figures) . . . . . . . . ....of Organic Material in the Kupferschiefer of the Lower Rhine Basin R. Diedel and W. Piittmann (with 7 Figures)...Langenstrassen F (1983) Neritic sedimentation of the Lower and Middle Devonian in the Rheinische Schiefergebirge...Field of the Fore-Sudetic Monocline (Southwestern Poland) S. SPECZIK J Abstract Fluid inclusion studies...rocks of the Fore-Sudetic Monocline of southwest Poland. Surprisingly high temperatures determined for |  | | Journal (article/letter/editorial) | | high-pressure/low-temperature rocks, fluid-mediated transport, serpentinite mélange, subduction processes This article’s...rocks (e.g., eclogite, blueschist) in exhumed serpentinite-matrix mélanges. Studies over the past ∼20...primarily jadeite composition (NaAlSi2 O6 ) Serpentinite: a rock composed principally of serpentine minerals...found in serpentinite boulder conglomerates and as veins and tectonic blocks in serpentinite. Although...(1984) in relationship to ophiolites (the term serpentinite mélanges should have been used, as discussed |  | | Report (issue) | | characteristics in limited exposures. Geologists working with lower grade rocks (Tull and Telle for example) attempt...Middle Ordovician age containing blocks of both Lower and Middle Ordovician carbonate rocks. Like the...and Berkshire Highlands. The line of isolated serpentinite bodies then stretches into Connecticut, where...Raymond and others (this volume) show that these amphibolite-facies and locally granulite-facies rocks contain...metavolcanic conglomerate facies in the Poor Mountain amphibolite and partly of lensoid slices of hanging-wall |  | | Book | | degrees of interaction between mantle-derived magmas, lower crustal felsic magmas, and, most likely, both mantle-...Formation). The area is metamorphosed up to the upper amphibolite facies (Abukuma type) and retro-metamorphosed...respectively. However, most elements are present in lower concentrations in the powdered sample set (H, C...metamorphic gradient of 500–700 ◦ C (e.g., [21]). Overall lower values of H, C, and N in the powdered Vietnamese...a quite strong asymmetric zoning with a layered lower unit composed by fine to medium grain size assemblage |  | | Report (issue) | | Yurkovich and Arthur J. Merschat STOP 2-3 Addie Quarry: Webster-Addie Mafic-ultramafic complex ...........P. Yurkovich STOP 2-4 Cartoogechaye terrane amphibolite on old U.S. 23-74 .............................sandstone and shale and some basalt flows in the lower Unicoi the Appalachians (Table 1). The remainder...Formation. represent the missing lower Tommotian interval—the Lower Ocoee Supergroup rocks filled a basin...sequence that The Ocoee Supergroup consists of the lower Snowbird Group has been correlated with the Cambro-Ordovician |  | Nokleberg, W.J., Aleinikoff, J.N., Lange, I.M., Silva, S.R., Miyaoka, R.T., Schwab, C.E., Zehner, R.E., Bond, G.C., Richter, D.H., Smith, T.E., Stout, J.H. (1992) Preliminary geologic map of the Mount Hayes Quadrangle, eastern Alaska Range, Alaska. Open-File Report Vol. 1992 (92-594) US Geological Survey doi:10.3133/ofr92594 | Report (issue) | | covered by undifferentiated colluvium (Qc). At lower elevations, deposits merge with and covered by undifferentiated...unconsolidated diamicton and boulder deposits. At lower elevations, consists chiefly of unconsolidated glaciofluvial...600 m. Locally divided into upper, middle, and lower members: Tsju Upper member Chiefly dark-gray mudstone...(jcs) of Jarvis Creek Glacier subterrane and the lower member (Tsjl) of the sedimentary rocks of Jarvis...stratigraphic thickness of 300 m or less Tsjl Lower member Chiefly angular quartz sandstone and conglomerate; |  | Reddy, K. Mahender, Mishra, Niharika, Simi, T. S., Rath, Sonali, Paul, Arijit, Sari, S. (2023) Special Publication Vol. 1-I (77), A Manual of the Geology of India : Precambrian Part I, Southern part of the peninsula (5th ed.) Geological Survey of India | Report (edition) | | 8 Ga) and Neoproterozoic (0.8 to 0.65 Ga). The lower and upper limits of these classified periods are...greenstones and related metasediments (greenschist- amphibolite facies) with voluminous granitoids belonging...supracrustals of lower amphibolite to granulite grade of metamorphosis whereas the Dharwars are of lower grade ranging...ranging from green schist to lower amphibolite facies of metamorphism. The southern strike extensions...facies, but gneisses and supracrustal rocks of amphibolite facies also do occur. Radiometric dates obtained |  | | Book | | LOESCHKE, H. HEINISCH The Pre-Alpine Basement of the Lower Austro-Alpine Nappes in the Bernina Massif (Grisons...its own, or it remained more or less fixed to its lower crust. 2. The sediments remained attached to their...Adriatic lower crust forced into the European plate (see Pfiffner this Vol.) exposed amphibolite-grade rocks...the Ivrea zone (Fig.3) which marks a part of the lower crust of the Apulian plate shortened during the...which results from gravity modelling, represents a lower constraint or the amount of shortening by thrust |  | | Book | | crystalline nappe complexes; the nappe units; 2 lower and less metamorphic MM Munchberg nappe complex;...area projection, Saxothuringian mica-schists near lower hemisphere) Neualbenreuth (A Lerchenbthl; B Froschfelsen...Moldanubian diagram Fabric (equal area projection, lower Zottbachtal hemisphere); (Fanger 1988) Bt probable...sillimanite-kspar (muscovite out) stability down to the lower greenschist facies. The peak of metamorphism coincides...(Klinkhammer and Rost 1975), both regarded as parts of lower nappe units. The trace element pattern of the Erbendorf |  | | Book (edition) | | molecules of the water are initially separated from the lower-energy molecules of the ice; this separation or...move predictably toward a more stable state of lower free energy. With regard to the second, it has been...readily attained at higher temperatures than at lower ones. This accords with our common experience that...NaA1SiO4 jadeite albite nepheline will favor the lower volume state. Hence P can influence the mineralogical...to be mechanically decoupled from the more rigid lower mantle. It is commonly assumed that the seismic |  | Nokleberg, Warren J., Parfenov, Leonid M., Khanchuk, Alexander I., Kuzmin, Mikhail I., Obolenskiy, Alexander A., Prokopiev, Andrei V., Rodionov, Sergey M., Smelov, Alexander P., Badarch, Gombosuren, Yan, Hongquan, Hwang, Duk-Hwan, Ogasawara, Masatsugu (2010) Appendix A: Description of the Northeast Asia Project and Associated Products. Professional Paper Vol. 1765 (1765a) US Geological Survey doi:10.3133/pp1765a | Report (issue) | | ic borate Sedimentary-metamorphic magnesite Serpentinite-hosted asbestos Talc (magnesite) replacement...metallogenic belts in the region (fig. 1) are the Kema, Lower Amur, and Popigay (fig. 4J; see appendix C). Two...replacement and granitoid-related deposits: the Kema and Lower Amur with Ag-Au epithermal vein, porphyry Cu-Mo...Mafic-ultramafic related Ti-Fe (+V) Podiform chromite Serpentinite-hosted asbestos Zoned mafic-ultramafic Cr-PGE...with ophiolitic complexes Podiform chromite Serpentinite-hosted asbestos C. Deposits associated with |  | Dril, Sergey, Khanchuk, Alexander I., Obolenskiy, Alexander A., Ogasawara, Masatsugu, Rodionov, Sergey M., Sotnikov, Vitaly I., Spiridonov, Alexander M., Seminsky, Zhan V., Timofeev, Vladimir F., Prokopiev, Andrei V., Nokleberg, Warren J. (2010) Late Carboniferous through early Jurassic metallogenesis and tectonics of northeast Asia, Chapter 7 in Metallogenesis and tectonics of northeast Asia. Professional Paper 1765_7. US Geological Survey doi:10.3133/pp17657 | Report (issue) | | ic borate Sedimentary-metamorphic magnesite Serpentinite-hosted asbestos Talc (magnesite) replacement...metallogenic belts in the region (fig. 1) are the Kema, Lower Amur, and Popigay (fig. 4J; see appendix C). Two...replacement and granitoid-related deposits: the Kema and Lower Amur with Ag-Au epithermal vein, porphyry Cu-Mo...Mafic-ultramafic related Ti-Fe (+V) Podiform chromite Serpentinite-hosted asbestos Zoned mafic-ultramafic Cr-PGE...with ophiolitic complexes Podiform chromite Serpentinite-hosted asbestos C. Deposits associated with |  | Rodionov, Sergey M., Obolenskiy, Alexander A., Distanov, Elimir G., Badarch, Gombosuren, Dejidmaa, Gunchin, Hwang, Duk-Hwan, Khanchuk, Alexander I., Ogasawara, Masatsugu, Nokleberg, Warren J., Parfenov, Leonid M., Prokopiev, Andrei V., Seminskiy, Zhan V., Smelov, Alexander P., Yan, Hongquan, Davydov, Yuriy V.V., Fridovskiy, Valeriy Yu., Gamyanin, Gennandiy N., Gerel, Ochir, Kostin, Alexei V., Letunov, Sergey A., Li, Xujun, Nikitin, Valeriy M., Ratkin, Vladimir V., Shpikerman, Vladimir I., Sudo, Sadahisa, Sotnikov, Vitaly I., Spiridonov, Alexander V., Stepanov, Vitaly A., Sun, Fengyue, Sun, Jiapeng, Sun, Weizhi, Supletsov, Valeriy M., Timofeev, Vladimir F., Tyan, Oleg A., Vetluzhskikh, Valeriy G., Wakita, Koji, Yakovlev, Yakov V., Zorina, Lydia M. (2010) Appendix C: Summary of Major Metallogenic Belts in Northeast Asia (the Russian Far East, Yakutia, Siberia, Transbaikalia, Northern China, Mongolia, South Korea, and Japan) Professional Paper Vol. 1765 (1765c) US Geological Survey doi:10.3133/pp1765c | Report (issue) | | ic borate Sedimentary-metamorphic magnesite Serpentinite-hosted asbestos Talc (magnesite) replacement...metallogenic belts in the region (fig. 1) are the Kema, Lower Amur, and Popigay (fig. 4J; see appendix C). Two...replacement and granitoid-related deposits: the Kema and Lower Amur with Ag-Au epithermal vein, porphyry Cu-Mo...Mafic-ultramafic related Ti-Fe (+V) Podiform chromite Serpentinite-hosted asbestos Zoned mafic-ultramafic Cr-PGE...with ophiolitic complexes Podiform chromite Serpentinite-hosted asbestos C. Deposits associated with |  | Rodionov, Sergey M., Khanchuk, Alexander I., Obolenskiy, Alexander A., Ogasawara, Masatsugu, Seminskiy, Zhan V., Prokopiev, Andrei V., Timofeev, Vladimir F., Nokleberg, Warren J. (2010) Middle Jurassic through Quaternary metallogenesis and tectonics of northeast Asia, Chapter 8 in Metallogenesis and tectonics of northeast Asia. Professional Paper 1765_8. US Geological Survey doi:10.3133/pp17658 | Report (issue) | | ic borate Sedimentary-metamorphic magnesite Serpentinite-hosted asbestos Talc (magnesite) replacement...metallogenic belts in the region (fig. 1) are the Kema, Lower Amur, and Popigay (fig. 4J; see appendix C). Two...replacement and granitoid-related deposits: the Kema and Lower Amur with Ag-Au epithermal vein, porphyry Cu-Mo...Mafic-ultramafic related Ti-Fe (+V) Podiform chromite Serpentinite-hosted asbestos Zoned mafic-ultramafic Cr-PGE...with ophiolitic complexes Podiform chromite Serpentinite-hosted asbestos C. Deposits associated with |  | Badarch, Gombosuren, Dejidmaa, Gunchin, Gerel, Ochir, Obolenskiy, Alexander A., Prokopiev, Andrei V., Timofeev, Vladimir F., Nokleberg, Warren J. (2010) Devonian through early Carboniferous (Mississippian) metallogenesis and tectonics of northeast Asia, Chapter 6 in Metallogenesis and tectonics of northeast Asia. Professional Paper 1765_6. US Geological Survey doi:10.3133/pp17656 | Report (issue) | | ic borate Sedimentary-metamorphic magnesite Serpentinite-hosted asbestos Talc (magnesite) replacement...metallogenic belts in the region (fig. 1) are the Kema, Lower Amur, and Popigay (fig. 4J; see appendix C). Two...replacement and granitoid-related deposits: the Kema and Lower Amur with Ag-Au epithermal vein, porphyry Cu-Mo...Mafic-ultramafic related Ti-Fe (+V) Podiform chromite Serpentinite-hosted asbestos Zoned mafic-ultramafic Cr-PGE...with ophiolitic complexes Podiform chromite Serpentinite-hosted asbestos C. Deposits associated with |  | Nokleberg, Warren J., Bundtzen, Thomas K., Dawson, Kenneth M., Eremin, Roman A., Goryachev, Nikolai A., Khanchuk, Alexander I., Monger, James W.H., Obolenskiy, Alexander A., Parfenov, Leonid M., Prokopiev, Andrei V., Ratkin, Vladimir V., Rodionov, Sergey M., Shpikerman, Vladimir I. (2010) Methodology of a combined regional metallogenic and tectonic analysis for northeast Asia, Chapter 2 in Metallogenesis and tectonics of northeast Asia. Professional Paper 1765_2. US Geological Survey doi:10.3133/pp17652 | Report (issue) | | ic borate Sedimentary-metamorphic magnesite Serpentinite-hosted asbestos Talc (magnesite) replacement...metallogenic belts in the region (fig. 1) are the Kema, Lower Amur, and Popigay (fig. 4J; see appendix C). Two...replacement and granitoid-related deposits: the Kema and Lower Amur with Ag-Au epithermal vein, porphyry Cu-Mo...Mafic-ultramafic related Ti-Fe (+V) Podiform chromite Serpentinite-hosted asbestos Zoned mafic-ultramafic Cr-PGE...with ophiolitic complexes Podiform chromite Serpentinite-hosted asbestos C. Deposits associated with |  | Berzin, Nikolai A., Distanov, Elimir G., Tomurtogoo, Onongyn, Timofeev, Vladimir F., Prokopiev, Andrei V., Nokleberg, Warren J. (2010) Neoproterozoic through Silurian metallogenesis and tectonics of northeast Asia, Chapter 5 in Metallogenesis and tectonics of northeast Asia. Professional Paper 1765_5. US Geological Survey doi:10.3133/pp17655 | Report (issue) | | ic borate Sedimentary-metamorphic magnesite Serpentinite-hosted asbestos Talc (magnesite) replacement...metallogenic belts in the region (fig. 1) are the Kema, Lower Amur, and Popigay (fig. 4J; see appendix C). Two...replacement and granitoid-related deposits: the Kema and Lower Amur with Ag-Au epithermal vein, porphyry Cu-Mo...Mafic-ultramafic related Ti-Fe (+V) Podiform chromite Serpentinite-hosted asbestos Zoned mafic-ultramafic Cr-PGE...with ophiolitic complexes Podiform chromite Serpentinite-hosted asbestos C. Deposits associated with |  | Smelov, Alexander P., Yan, Hongquan, Timofeev, Vladimir F., Prokopiev, Andrei V., Nokleberg, Warren J. (2010) Archean through Mesoproterozoic metallogenesis and tectonics of northeast Asia, Chapter 4 in Metallogenesis and tectonics of northeast Asia. Professional Paper 1765_4. US Geological Survey doi:10.3133/pp17654 | Report (issue) | | ic borate Sedimentary-metamorphic magnesite Serpentinite-hosted asbestos Talc (magnesite) replacement...metallogenic belts in the region (fig. 1) are the Kema, Lower Amur, and Popigay (fig. 4J; see appendix C). Two...replacement and granitoid-related deposits: the Kema and Lower Amur with Ag-Au epithermal vein, porphyry Cu-Mo...Mafic-ultramafic related Ti-Fe (+V) Podiform chromite Serpentinite-hosted asbestos Zoned mafic-ultramafic Cr-PGE...with ophiolitic complexes Podiform chromite Serpentinite-hosted asbestos C. Deposits associated with |
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