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Littérature scientifique sur le sujet « Metamorphic Metamorphism (Geology) »

Auteur : Grafiati

Publié le 4 juin 2021

Mis à jour le 9 février 2022

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Articles de revues sur le sujet "Metamorphic Metamorphism (Geology)"

1

Brown, Michael. « Metamorphic geology : Tectonics of metamorphism ». Nature 318, n^o 6044 (novembre 1985) : 314–15. http://dx.doi.org/10.1038/318314a0.

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Li, Zhen, Hao Wang, Qian Zhang, Meng-Yan Shi, Jun-Sheng Lu, Jia-Hui Liu et Chun-Ming Wu. « Ultra-High Pressure Metamorphism and Geochronology of Garnet Clinopyroxenite in the Paleozoic Dunhuang Orogenic Belt, Northwestern China ». Minerals 11, n^o 2 (24 janvier 2021) : 117. http://dx.doi.org/10.3390/min11020117.

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Ultra-high pressure (UHP) metamorphism is recorded by garnet clinopyroxenite enclaves enclosed in an undeformed, unmetamorphosed granitic pluton, northeastern Paleozoic Dunhuang orogenic belt, northwestern China. The protoliths of the garnet clinopyroxenite might be basic or ultrabasic volcanic rocks. Three to four stages of metamorphic mineral assemblages have been found in the garnet clinopyroxenite, and clockwise metamorphic pressure–temperature (P-T) paths were retrieved, indicative of metamorphism in a subduction environment. Peak metamorphic P-T conditions (790–920 °C/28–41 kbar) of garnet clinopyroxenite suggest they experienced UHP metamorphism in the coesite- or diamond-stability field. The UHP metamorphic event is also confirmed by the occurrence of high-Al titanite enclosed in the garnet, along with at least three groups of aligned rutile lamellae exsolved from the garnet. Secondary ion mass spectrometry (SIMS) U-Pb dating of metamorphic titanite indicates that the post-peak, subsequent tectonic exhumation of the UHP rocks occurred in the Devonian period (~389–370 Ma). These data suggest that part of the Paleozoic Dunhuang orogenic belt experienced UHP metamorphism, and diverse metamorphic facies series prevailed in this Paleozoic orogen. It can be further inferred that most of the UHP rocks in this orogen remain buried.

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MAJKA, JAROSLAW, STANISLAW MAZUR, MACIEJ MANECKI, JERZY CZERNY et DANIEL K. HOLM. « Late Neoproterozoic amphibolite-facies metamorphism of a pre-Caledonian basement block in southwest Wedel Jarlsberg Land, Spitsbergen : new evidence from U–Th–Pb dating of monazite ». Geological Magazine 145, n^o 6 (10 septembre 2008) : 822–30. http://dx.doi.org/10.1017/s001675680800530x.

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AbstractSouthwest Spitsbergen, Wedel Jarlsberg Land, consists of two Proterozoic crustal blocks with differing metamorphic histories. Both blocks experienced Caledonian greenschist-facies metamorphism, but only the southern block records an earlier pervasive M1 amphibolite-facies metamorphism and strong deformational fabric. In situ EMPA total-Pb monazite geochronology from both matrix and porphyroblast inclusion results indicate that the older M1 metamorphism occurred at 643 ± 9 Ma, consistent with published cooling ages of c. 620 Ma (hornblende) and 580 Ma (mica) obtained from these same rocks. This region thus contains a lithostratigraphic profile and metamorphic history which are unique within the Svalbard Archipelago. Documentation of a pervasive late Neoproterozoic Barrovian metamorphism is difficult to reconcile with a quiescent non-tectonic regime typically inferred for this region, based on the occurrence of rift-drift sequences on the Baltic and Laurentian passive margins. Instead, our new metamorphic age implies an exotic origin of the pre-Devonian basement exposed in SW Spitsbergen and supports models of terrane assembly postulated for the Svalbard Archipelago.

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Lardeaux, Jean-Marc. « Deciphering orogeny : a metamorphic perspective. Examples from European Alpine and Variscan belts ». Bulletin de la Société Géologique de France 185, n^o 2 (1 février 2014) : 93–114. http://dx.doi.org/10.2113/gssgfbull.185.2.93.

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AbstractIn this paper we review and discuss, in a synthetic historical way, the main results obtained on Alpine metamorphism in the western Alps. First, we describe the finite metamorphic architecture of the western Alps and discuss its relationships with subduction and collision processes. Second, we portray the progressive metamorphic evolution through time and space with the presentation of 5 metamorphic maps corresponding to critical orogenic periods, namely 85-65 Ma, 60-50 Ma, 48-40 Ma, 38-33 Ma and 30-20 Ma. We underline the lack of temporal data on high-pressure/low-temperature metamorphic rocks as well as the severe uncertainties on the sizes of rock units that have recorded the same metamorphic history (i.e. coherent P-T-t/deformation trajectories). We discuss the role of subduction-driven metamorphism in ocean-derived protoliths and the conflicting models that account for the diachrony of continental subductions in the western Alps.

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Prakash, D., DK Patel, MK Yadav, B. Vishal, S. Tewari, R. Yadav, SK Rai et CK Singh. « Prograde polyphase regional metamorphism of pelitic rocks, NW of Jamshedpur, eastern India : constraints from textural relationship, pseudosection modelling and geothermobarometry ». Geological Magazine 157, n^o 7 (11 novembre 2019) : 1045–67. http://dx.doi.org/10.1017/s0016756819001171.

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AbstractThe study area belongs to the Singhbhum metamorphic belt of Jharkhand, situated in the eastern part of India. The spatial distribution of the index minerals in the pelitic schists of the area shows Barrovian type of metamorphism. Three isograds, viz. garnet, staurolite and sillimanite, have been delineated and the textural study of the schists has revealed a time relation between crystallization and deformation. Series of folds with shifting values of plunges in the supracrustal rocks having axial-planar schistosity to the folds have been widely cited. Development of these folds could be attributed to the second phase of deformation. In total, two phases of deformation, D1 and D2, in association with two phases of metamorphism, M1 and M2, have been lined up in the study area. Chemographic plots of reactant and product assemblages corresponding to various metamorphic reactions suggest that the pattern of metamorphic zones mapped in space is in coherence with the temporal-sequential change during prograde metamorphism. The prograde P–T evolution of the study area has been obtained using conventional geothermobarometry, internally consistent winTWQ program and Perple_X software in the MnNCKFMASHTO model system. Our observations suggest that the progressive metamorphism in the area is not related to granitic intrusion or migmatization but that it was possibly the ascending plume that resulted in the M1 phase of metamorphism followed by D1 deformation. The second and prime metamorphic phase, M2, with its possible heat source generated by crustal overloading, was preceded by D1 and it lasted until late- to post-D2 deformation.

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Biševac, Vanja, Kadosa Balogh, Dražen Balen et Darko Tibljaš. « Eoalpine (Cretaceous) very low- to low-grade metamorphism recorded on the illite-muscovite-rich fraction of metasediments from South Tisia (eastern Mt Papuk, Croatia) ». Geologica Carpathica 61, n^o 6 (1 décembre 2010) : 469–81. http://dx.doi.org/10.2478/v10096-010-0029-9.

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Eoalpine (Cretaceous) very low- to low-grade metamorphism recorded on the illite-muscovite-rich fraction of metasediments from South Tisia (eastern Mt Papuk, Croatia)Eoalpine very low- to low-grade metamorphism related to Cretaceous orogenesis has been investigated in the Slavonian Mts, Croatia. Samples belonging to the Psunj metamorphic complex (PMC), the Radlovac metamorphic complex (RMC) and Permian-Triassic and Triassic sedimentary sequences (PTSS) were studied. The Kübler and Árkai indices of all the analysed samples indicate high-anchizonal to epizonal metamorphism. The degree of Eoalpine metamorphism tends to be constant in all samples implying that the different complexes passed through and recorded the same event. Measurements of illite-white K-micab0-parameter of the RMC samples imply transitional low- to medium-pressure character of the metamorphism. These data together with K-Ar ages (~100-80 Ma) measured on illite-white K-mica rich < 2 μm grain-size fractions point to Late Cretaceous very low- to low-grade regional metamorphism presumably related to the main nappe-forming compressional events in the Pannonian Basin and the Carpathians. The P-T-t (pressure-temperature-time) evolution of the studied area is in good agreement with similar scenarios in the surrounding areas of Tisia, but also in Eastern Alps, Carpathians and Pannonian Basin (ALCAPA).

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APARICIO, A., M. A. BUSTILLO, R. GARCIA et V. ARAÑA. « Metasedimentary xenoliths in the lavas of the Timanfaya eruption (1730–1736, Lanzarote, Canary Islands) : metamorphism and contamination processes ». Geological Magazine 143, n^o 2 (mars 2006) : 181–93. http://dx.doi.org/10.1017/s0016756806001713.

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We report on the investigation of contact metamorphism provoked by the emplacement of a shallow magma chamber during the Timanfaya eruption of Lanzarote from 1730 to 1736 AD. The study was carried out on metamorphic xenoliths from basaltic Timanfaya lavas, and shows how the primary basanitic magma was contaminated by sedimentary and metamorphic rocks. Mineralogical and chemical studies allowed the definition of several xenolith types. Silica xenoliths (quartz, tridymite, cristobalite or a mixture of these, constituting more than 50 % of the xenolith) and calc-silicate xenoliths (wollastonite, sometimes the 2M type, diopside, forsterite or mixture of these, constituting more than 50 % of the xenolith) are the most frequent. Other minerals recognized were calcite, dolomite, augite, enstatite, hypersthene, spinel and scapolite. The mineralogy and some textures of the metamorphic forsteritic xenoliths are identical to those found in ultrabasic xenoliths (dunites) and point to a possible metamorphic origin for some of them. Major and trace elements showed a diversity of composition, controlled by the mineralogy. The REE composition of the metamorphic xenoliths is high, compared with the sedimentary xenoliths not affected by metamorphism. The mineral assemblages define metamorphic facies of low, medium and high grade, depending on the distance of the sedimentary rocks from the magma chamber border. The IGPETWIN-MIXING program was used to verify the contamination process, taking the xenoliths as representative of the sedimentary/metamorphic rocks that were melted. The results indicated that sedimentary/metamorphic rock contamination of a basanitic magma can produce tholeiitic compositions.

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Dallmeyer, R. D. « Partial thermal resetting of 40Ar/39Ar mineral ages in western Spitsbergen, Svalbard : possible evidence for Tertiary metamorphism ». Geological Magazine 126, n^o 5 (septembre 1989) : 587–93. http://dx.doi.org/10.1017/s001675680002286x.

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AbstractHornblende and muscovite within high-grade Caledonian metamorphic rocks exposed in Albert I Land (northwest Spitsbergen) display internally concordant 40Ar/39Ar age spectra providing no record of any post-Silurian thermal history. Both minerals record 420−425 Ma plateau ages indicating that relatively rapid cooling followed Silurian metamorphism. Muscovite within some metamorphic sequences exposed within the Tertiary tectonic zone of Oscar II Land (west-central Spitsbergen) displays a low-temperature 40Ar/39Ar age spectra discordance suggestive of a slight, post-Caledonian thermal disturbance. This is consistent with a post-Palaeozoic thermal overprint documented elsewhere in Oscar II Land and indicates that, at least locally, metamorphism may have accompanied the Tertiary orogeny.

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Hara, Hidetoshi, Hiroshi Mori, Kohei Tominaga et Yuki Nobe. « Progressive Low-Grade Metamorphism Reconstructed from the Raman Spectroscopy of Carbonaceous Material and an EBSD Analysis of Quartz in the Sanbagawa Metamorphic Event, Central Japan ». Minerals 11, n^o 8 (8 août 2021) : 854. http://dx.doi.org/10.3390/min11080854.

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Low-grade metamorphic temperature conditions associated with the Sanbagawa metamorphic event were estimated by the Raman spectroscopy of carbonaceous material (RSCM) in pelitic rocks and an electron backscatter diffraction (EBSD) analysis of the quartz in siliceous rocks. Analytical samples were collected from the Sanbagawa metamorphic complex, the Mikabu greenstones, and the Chichibu accretionary complex in the eastern Kanto Mountains, central Japan. Previously, low-grade Sanbagawa metamorphism was only broadly recognized as pumpellyite–actinolite facies assigned to the chlorite zone. The RSCM results indicate metamorphic temperatures of 358 °C and 368 °C for the chlorite zone and 387 °C for the garnet zone of the Sanbagawa metamorphic complex, 315 °C for the Mikabu greenstones, and 234–266 °C for the Chichibu accretionary complex. From the EBSD analyses, the diameter of the quartz grains calculated by the root mean square (RMS) approximation ranges from 55.9 to 69.0 μm for the Sanbagawa metamorphic complex, 9.5 to 23.5 μm for the Mikabu greenstones, and 2.9 to 7.3 μm for the Chichibu accretionary complex. The opening angles of the c-axis fabric approximate 40–50°, presenting temperatures of 324–393 °C for the Sanbagawa metamorphic complex and the Mikabu greenstones. The temperature conditions show a continuous increase with no apparent gaps from these low-grade metamorphosed rocks. In addition, there exists an empirical exponential relationship between the estimated metamorphic temperatures and the RMS values of the quartz grains. In this study, integrated analyses of multiple rock types provided valuable information on progressive low-grade metamorphism and a similar approach may be applied to study other metamorphic complexes.

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Talarico, F. M., E. Stump, B. F. Gootee, K. A. Foland, R. Palmeri, W. R. Van Schmus, P. K. Brand et C. A. Ricci. « First evidence of a “Barrovian”-type metamorphic regime in the Ross orogen of the Byrd Glacier area, central Transantarctic Mountains ». Antarctic Science 19, n^o 4 (2 août 2007) : 451–70. http://dx.doi.org/10.1017/s0954102007000594.

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AbstractThe Selborne Group comprises two metamorphic rock units, the muscovite±dolomite bearing Madison Marble and the biotite-muscovite±quartz-calcite Contortion Schist, which contains thick lenses of variably deformed metabasalts and metaconglomerates. Petrological and structural data indicate a polyphase metamorphic evolution including: i) an early stage of upper greenschist regional metamorphism (P = ~0.15–0.3 GPa; T = ~380–450°C), ii) prograde metamorphism during D1 up to amphibolite facies peak conditions (P = 0.58–0.8 GPa, T = ~560–645°C), iii) syn-D2 unloading-cooling retrograde metamorphism, iv) a post-D2 contact metamorphic overprint at variable T between 450 and 550°C and ~0.2 GPa connected to the emplacement of granitic plutons and felsic dyke swarms. Geochronological data constrain the polyphase syn-D1/D2 evolution between ~ 510 and 492 Ma. A similar metamorphic path, including a medium P stage but at lower T conditions, is documented in greenschist facies metabasalts within the Byrd Group in the Mount Dick area. The metamorphic pattern and close lithostratigraphic matching between Selborne Group and Byrd Group sharply contrast with the high-grade Horney Formation that is exposed north of the Byrd Glacier and corroborate the hypothesis that the Byrd Glacier discontinuity marks a first-order crustal tectonic boundary crossing the Ross orogen.

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Thèses sur le sujet "Metamorphic Metamorphism (Geology)"

1

Rougvie, James Russell. « Metamorphism in the northern Park Range of Colorado : fluid-rock interactions and thermobarometry / ». Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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Standley, Carl E. « Banda forearc metamorphic rocks accreted to the Australian continental margin : detailed analysis of the Lolotoi Complex of East Timor / ». Diss., CLICK HERE for online access, 2007. http://contentdm.lib.byu.edu/ETD/image/etd1696.pdf.

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3

Cui, Xiaojun. « Numerical modeling of reactive fluid flow in the Notch Peak contact metamorphic aureole, Utah / ». free to MU campus, to others for purchase, 2002. http://wwwlib.umi.com/cr/mo/fullcit?p3060092.

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Walker, James David. « The structure and metamorphic evolution of the High Himalayan Slab in SE Zanskar and NW Lahaul ». Thesis, University of Oxford, 1998. http://ora.ox.ac.uk/objects/uuid:fc8b8fd3-e155-4f2f-9256-3667c2b31f4f.

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This thesis attempts to unravel the complex thermal and structural history of part of the High Himalayan Slab in NW India and combines reconnaissance-style field structural mapping of an area covering ~10,000 km² with petrography, microstructural analysis, thermobarometry and geochronology techniques. The results of this work show that the oldest protoliths of the High Himalayan Slab are at least Cambrian in age and that they may have experienced a major pre-Himalayan metamorphism at c.500 Ma. The youngest protoliths are Mesozoic in age (the Tandi Group) and demonstrate that the High Himalayan Slab represents the metamorphosed equivalents of the Tibetan Sedimentary Series. Metamorphism was achieved via substantial crustal shortening and thickening following the India-Asia collision at 50-54 Ma ago. Phase relationships demonstrate that metamorphism was a regional Barrovian-type event associated with the growth of biotite-, garnet-, staurolite-, kyanite- and sillimanite-bearing assemblages in metapelites. Quantitative thermobarometry demonstrates that near-peak conditions of c.6-8 kbar and 550-650°C were attained in the deepest exposed levels. Growth of metamorphic assemblages was underway by at least 30 Ma, as indicated by U-Pb ages of metamorphic monazites. Exhumation of the High Himalayan Slab was achieved through a combination of extensional unroofing along major detachments (namely the Zanskar Shear Zone), thermal doming, thrusting along the Main Central Thrust and surface erosion. Exhumation is closely associated with the growth of sillimanite- and cordierite-bearing assemblages in pelites and the generation and emplacement of crustal melt leucogranites in the upper parts of the slab. U-Pb dating of accessory phases from one of the crustal melt leucogranites (the Gumburanjon leucogranite) constrains its crystallisation and emplacement age at c.21-22 Ma. This is only slightly older than its ⁴⁰Ar/³⁹Ar muscovite and biotite cooling ages of c.20-21 Ma, which is attributed to the emplacement of the Gumburanjon leucogranite into the immediate footwall of the ZSZ. Field and geochronological data therefore support a strong temporal and spatial relationship between upper crustal melting and extension in a convergent orogen.

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Ambrose, Tyler. « Structure, metamorphism, and tectonics of the northern Oman-UAE ophiolite and underlying metamorphic sole ». Thesis, University of Oxford, 2017. http://ora.ox.ac.uk/objects/uuid:e9520624-0f91-4c9d-a9b9-e9e2fc5d5517.

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Ophiolites - thrust sheets of oceanic lithosphere that have been emplaced onto the continental margin - provide the opportunity to explore the structure and genesis of oceanic crust. As many ophiolites formed above subduction zones, they also allow for the investigation of mantle wedge and subduction interface processes. This the- sis examines the Oman-United Arab Emirates (UAE) ophiolite, which is the largest and most intensely studied ophiolite on Earth. Three distinct problems are addressed. (1) Recent research has proposed that the architecture and tectonic evolution of the ophiolite in the UAE differs from in Oman. In Chapter 2, I test this hypothesis by integrating new geological mapping and field observations with previously published maps of the ophiolite in the UAE. My results indicate that the ophiolite is gently folded, but otherwise largely intact. I demonstrate that the architecture of the ophi- olite in the UAE is not significantly different from in Oman. Thus, there is no basis for a different tectonic evolution as recently proposed. (2) Observations from exper- iments and small-scale natural shear zones indicate that volumetrically-minor phases can control strain localization. In Chapter 3, I test the hypothesis that minor phases control strain-localisation at plate boundaries. To do so, I analyzed peridotites from the base of the ophiolite, a palaeosubduction interface. My results demonstrate that minor phases limited olivine grain growth, which led to rheological weakening. (3) The mechanisms by which metamorphic soles detached from the downgoing slab and accreted to the hanging-wall mantle is unclear. In Chapter 4, I examine a transect across the metamorphic sole in the UAE. My results reveal that granulite formation was more extensive than is typically considered. I propose that granulite formation resulted in rheological strengthening, which caused the subduction interface to migrate into the downgoing slab and accrete the metamorphic sole.

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Strowbridge, Susan Leah. « Metamorphic evolution of anatectic metapelites from the Gabriel high strain zone, Grenville Province / ». Internet access available to MUN users only, 2005. http://collections.mun.ca/u?/theses,62592.

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Baker, Andrew James. « Metamorphic studies in the Scottish Highlands ». Thesis, University of Oxford, 1985. http://ora.ox.ac.uk/objects/uuid:0000df07-a390-4b43-af48-31f04ba628ec.

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Conditions of 8kb and 800°C are estimated for sillimanite K feldspar bearing metapelites and garnet-clinopyroxene bearing amnphibolites in Glen Muick. These conditions are inconsistent with the simultaneous nearby presence of equilibrium between andalusite and kyanite. Andalusite in the Glen Muick area is late. The sillimanite zone may have been in part primary. There is a transition without major structural break between Tay Nappe flat belt and the "Banff Nappe". A dataset has been derived for phases in the system KCMASHCO₂. The MHSRK equation of Kerrick and Jacobs (1981) has been used to extract data from mixed devolatilisation equilibria. Heats of formation are in agreement with calorimetrically determined values. Phlogopite equilibria calculated using disordered phlogopite data seem most appropriate to natural metapelite assemblages. Variations in pressure and temperature have been constrained across the Dalradian using various calibrated reactions. Temperatures vary from about 500°C in the low kyanite zone to 800°C in the sillimanite-K feldspar zone and pressures vary from 4kb to 10kb. Pressure estimates are justified on the basis that they are consistent with the aluminosilicate phase diagram. Rocks from the Central Highlands to Glen Clova underwent a decrease in pressure during evolution through peak metamorphic conditions. Amphibolites from the southern Moines show evidence of a former eclogitic assemblage of early Grampian age or earlier. High temperature regional metamorphic rocks lie at high structural levels and are are suggested to be an allochthonous unit, the Banff Nappe of Grampian age. The western margin of the Banff Nappe is marked by a temperature maximum to the immediate east, sharp thermal transitions, a train of metabasites and a high strain zone. It is suggested that emplacement of a Banff Nappe resulted in the deformation and metamorphism of structurally lower rocks.

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Huff, Timothy A. « Fluid inclusion evidence for metamorphic fluid evolution in the Black Hills, South Dakota / ». free to MU campus, to others for purchase, 2004. http://wwwlib.umi.com/cr/mo/fullcit?p1421144.

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Miller, Martin Gregg. « Structural and kinematic evolution of the Badwater Turtleback, Death Valley, California / ». Thesis, Connect to this title online ; UW restricted, 1992. http://hdl.handle.net/1773/6716.

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Tollefsen, Elin. « Thermal and chemical variations in metamorphic rocks in Nautanen, Gällivare, Sweden ». Thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2014. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-149643.

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This study focuses on the geology of the Nautanen area. It is part of the SGU-financed project, Metamorphic Map of Sweden, which aims to compile metamorphic data from Sweden and takes the form of a number of Bachelor and Master projects. The main metamorphic event in the Nautanen area is the Svecokarelian Orogeny (1.96 – 1.75 Ga). The samples are metamorphosed sedimentary and volcanic rocks, which were intruded by intermediate to mafic intrusions and a later granite intrusion. The supracrustal rocks are folded and the Nautanen Deformation Zone (NDZ) traverses the area in a NW to SE direction. Petrographic studies, XRF analysis and THERMOCALC were used to estimate pressure and temperature and to elucidate evidence of fluid mobility. The average pressure was assumed to be below 4 kbar because of the presence of andalusite. The lowest and highest temperatures for metamorphism were 474±43°C and 681±14°C, with highest temperatures recorded nearest to the granite intrusion. XRF analysis revealed high concentrations of Ba (up to 7000 ppm) in the NDZ. High concentrations of Ba, skarn formation and replacement of garnet by chlorite indicate fluid-controlled metamorphism in the NDZ. The increasing temperature towards the granite intrusion suggests regional or contact prograde metamorphism that need not be related to the NDZ.
Metamorphic Map of Sweden, SGU-project

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Livres sur le sujet "Metamorphic Metamorphism (Geology)"

1

Liu, Xishan. Metamorphic geology. Changchun Shi : Jilin University Pub. House, 2001.

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2

Steltenpohl, Mark G. Metamorphism in the Alabama Piedmont. Tuscaloosa, Ala. (420 Hackberry Lane, P.O. Box 0, Tuscaloosa 35486-9780) : Geological Survey of Alabama, Mineral Resources Division, 1988.

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Reenen, D. D. Van. Metamorfose : Die sleutel tot die herkenning van oer gebiede van bergbouing. Johannesburg : Randse Afrikaanse Universiteit, 1988.

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4

Metamorphic crystallization. Chichester, Sussex, England : J. Wiley, 1994.

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5

Dusel-Bacon, Cynthia. Metamorphic history of Alaska. Menlo Park, CA : U.S. Geological Survey, 1991.

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6

Jing ji bu Zhong yang di zhi diao cha suo (China), dir. Taiwan de bian zhi yan. Taibei Xian Zhonghe Shi : Jing ji bu Zhong yang di zhi diao cha suo, 1998.

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Dusel-Bacon, Cynthia. Distribution, facies, ages, and proposed tectonic associations of regionally metamorphosed rocks in southwestern Alaska and the Alaska Peninsula. Washington : U.S. G.P.O., 1996.

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Dusel-Bacon, Cynthia. Metamorphic facies map of southeastern Alaska : Distribution, facies, and ages of regionally metamorphosed rocks. Washington : U.S. G.P.O., 1996.

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9

Visser, Diederik. The metamorphic evolution of the Bamble sector, south Norway : A paragenetic and mineral chemical study of cordierite-orthoamphibole-bearing rocks with special reference to borosilicate-bearing mineral assemblages. [Utrecht : Faculteit Aardwetenschappen der Rijksuniversiteit Utrecht, 1993.

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Metamorphic rocks and their geodynamic significance : A petrological handbook. Dordrecht : Kluwer Academic Publishers, 2002.

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Chapitres de livres sur le sujet "Metamorphic Metamorphism (Geology)"

1

Quesada, C., et J. Munha. « Metamorphism ». Dans Pre-Mesozoic Geology of Iberia, 314–20. Berlin, Heidelberg : Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-83980-1_20.

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Santallier, D. S., J. M. Lardeaux, J. Marchand et Ch Marignac. « Metamorphism ». Dans Pre-Mesozoic Geology in France and Related Areas, 324–40. Berlin, Heidelberg : Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-84915-2_28.

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Dercourt, Jean, et Jacques Paquet. « Metamorphic Rocks ». Dans Geology Principles & ; Methods, 81–97. Dordrecht : Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4956-0_6.

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McCann, Tom. « Metamorphic Rocks ». Dans Pocket Guide Geology in the Field, 99–118. Berlin, Heidelberg : Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-63082-2_4.

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Ribeiro, M. L., J. Reche, A. López-Carmona, C. Aguilar, T. Bento dos Santos, M. Chichorro, Í. Dias da Silva et al. « Variscan Metamorphism ». Dans The Geology of Iberia : A Geodynamic Approach, 431–95. Cham : Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10519-8_12.

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Massonne, H. J. « Metamorphic Evolution ». Dans Pre-Permian Geology of Central and Eastern Europe, 132–37. Berlin, Heidelberg : Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-77518-5_12.

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Okrusch, M. « Metamorphic Evolution ». Dans Pre-Permian Geology of Central and Eastern Europe, 201–13. Berlin, Heidelberg : Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-77518-5_21.

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Blümel, P. « Metamorphic Evolution ». Dans Pre-Permian Geology of Central and Eastern Europe, 260–65. Berlin, Heidelberg : Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-77518-5_26.

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Blümel, P. « Metamorphic Evolution ». Dans Pre-Permian Geology of Central and Eastern Europe, 295–308. Berlin, Heidelberg : Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-77518-5_29.

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Kryza, R. « Metamorphic Evolution ». Dans Pre-Permian Geology of Central and Eastern Europe, 351–59. Berlin, Heidelberg : Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-77518-5_34.

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Actes de conférences sur le sujet "Metamorphic Metamorphism (Geology)"

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Parcher, Sara, Harmon Maher et Tim F. Redfield. « GEOLOGIC HISTORY OF A METAMORPHIC CORE COMPLEX IN NW SPITSBERGEN ». Dans Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-327442.

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Rangel, Diana Nunez, Oriani Reyes Santiago, Angelica Nino Rodriguez, Alejandro Franco Rojas et Edgar Alexander Padilla Gonzalez. « Correlation Between Morphometric Parameters and Geology of Igneous and Metamorphic Basins in Colombia ». Dans 2020 Congreso Internacional de Innovación y Tendencias en Ingeniería (CONIITI). IEEE, 2020. http://dx.doi.org/10.1109/coniiti51147.2020.9240314.

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Aronoff, Ruth F., Jeffrey D. Vervoort et Jade-Ashley Carberry. « ADDING DETAIL TO A GEOLOGIC MAP USING GEOCHRONOLOGY AND METAMORPHIC MODELING TOOLS ». Dans GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-325018.

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Fadda, Sandro. « GENETIC ASPECTS OF TALC-CHLORITE FORMATION IN CENTRAL SARDINIA, ITALY : METAMORPHISM, HYDROTHERMALISM AND MG-METASOMATISM : THE CASE OF SA MATTA AND SU VENOSU MINES ». Dans 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b11/s1.013.

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Henry, Darrell J., et Barbara L. Dutrow. « COURSE-EMBEDDED RESEARCH AND SCIENTIFIC COMMUNICATIONS IN UNDERGRADUATE GEOLOGY MAJORS COURSES : EXAMPLES FROM THE MINERALOGY – IGNEOUS/METAMORPHIC PETROLOGY SEQUENCE AT LSU ». Dans GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298440.

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González-León, Carlos M., Teresita Sánchez, Michelle Vázquez, Luigi Solari, Jonathan A. Nourse, Ricardo Amaya-Martínez et Angel Zapata Martínez. « GEOLOGY AND LA-ICPMS U-PB GEOCHRONOLOGY OF THE WESTERN LOWER PLATE OF THE MAGDALENA-MADERA METAMORPHIC CORE COMPLEX, NORTHERN SONORA, MEXICO ». Dans Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-313994.

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Tollefson, Kyle T., Barbara L. Dutrow et Darrell J. Henry. « CATHODOLUMINESCENCE (CL) RESPONSE OF FELDSPARS IN MULTIPLE VEINS SETS AS A MEANS TO IDENTIFY SOURCE REGION : IMPLICATIONS FOR GEOLOGIC EVOLUTION OF THE SAWTOOTH METAMORPHIC COMPLEX, ID, USA ». Dans GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-335779.

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Yu, Jingfeng, Diao Zhou, Bo Zhang, Haiping Meng, Tong Li, Li Wang, Yong Wang et al. « Horizontal Well Drilling and Geosteering Optimization with Integrated Innovation Technologies : Case Studies from the World Largest Conglomerate Reservoir in West China ». Dans International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21482-ms.

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Abstract MH oilfield is a fan delta deposited unconventional tight oil reservoir with complex lithology of volcanic rocks, metamorphic rocks, conglomerate, and claystone. The drilling efficiency was optimized by using the first-generation boundary mapping technology with Rotary Steering System (RSS) during the first batch drilling campaign (H2-2016∼H1-2017), which was mentioned in IADC/SPE-190998-MS. But with the development going further, more and more wells drilled into shale interbed causing low pay zone exposure, long drilling duration, and numerous drilling hazards. The overall drilling performance was not optimistic as before, the average Rate Of Penetration (ROP) decreased by 30.7% and the average footage per run decreased by 38.9% during horizontal section operation in some specific blocks of MH oilfield. By reviewing the detailed drilling and geology material of the first batch drilling, the challenges were defined. There is lateral irregular thin shale interbed existing in this conglomeratic reservoir which is rarely observed from the nearby wells in the first batch drilling zone. That unstable shale interbed with 0.5-2m thickness isolated the target into 2 to 3 components. The first-generation boundary mapping technology can only detect the nearest up or down boundary, with this limitation, it is difficult to reveal these laterally unstable shale interbed. It is crucial to precisely delineate the irregular thin interbed to develop this complex reservoir. Meanwhile, the bit selection which didn't catch up with the formation change is another issue that needs to be optimized timely. To solve the above challenges, the new generation boundary mapping while drilling technology was introduced to this project, it has 3 or more boundaries detecting ability at the same time, which can delineate the irregular thin interbed and optimize real-time Well Placement decision making. Meanwhile, the bit design and selection based on the timely geological data interpretation helped to improve drilling efficiency. This innovative integrated method deployed in phase II horizontal well drilling campaign proved to be an effective approach to optimize geosteering and drilling performance. The clear reservoir geometry delineation effectively helps avoid entering the irregular shale interbed in real-time, thus improve the pay zone exposure and trajectory smoothness. Till 2018, more than 50 wells were completed, the overall drilling performance of 2018 has been improved by 47.2% of footage per run and 42.2% of ROP compared with statistical results of H2-2017 of the M131 block and nearly back to the normal level. In this paper, the authors will demonstrate how this integrated approach helps optimize Well Placement, enhance drilling efficiency and save budget with some exemplary case studies. With this success, the authors believe this approach and techniques could effectively address the following horizontal well drilling campaign in this unconventional tight oil reservoir.

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Rapports d'organisations sur le sujet "Metamorphic Metamorphism (Geology)"

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Gareau, S. A. Geology, Scotia-Quaal Metamorphic Belt, Coast Plutonic Complex, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/209259.

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Gareau, S. A. Geology of the Scotia - Quaal Metamorphic Belt, Coast Plutonic Complex, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131690.

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Israel, S. A., et L. A. Kennedy. Geology of the Atnarko metamorphic complex, southern Tweedsmuir Park, west-central British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214020.

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Rogers, H. D. Geology of the igneous-metamorphic complex of Shelburne and eastern Yarmouth counties, Nova Scotia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120203.

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Burgess, J. L., M. Brown et C. R. van Staal. Preliminary report on the metamorphic geology of the Port aux Basques Complex, southwestern Newfoundland. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132891.

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Grover, T. W., M. R. McDonough et V. J. McNicoll. Preliminary report on the metamorphic geology of Taltson Magmatic Zone, Canadien Shield, northeastern Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/134249.

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Israel, S. A., et L. A. Kennedy. Reconnaissance of structural geology of the Atnarko metamorphic complex, southern Tweedsmuir Park, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213078.

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Sanborn-Barrie, M., T. Skulski, H. Sandeman, R. Berman, S. Johnstone, T. MacHattie et D. Hyde. Structural and metamorphic geology of the Walker Lake-Arrowsmith River area, Committee Bay belt, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213187.

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Sandeman, H. A., C. Studnicki-Gizbert, J. Brown et S. Johnstone. Regional structural and metamorphic geology of the Committee Bay Belt, Laughland Lake area, central mainland, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212091.

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Tallman, P., A. Sangster et R. A. Jamieson. Geology and mineralization of the Jumping Brook metamorphic suite, Faribault Brook area, western Cape Breton Island, Nova Scotia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122427.

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