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  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 212 (1966), S. 676-678 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] FLUORINE is often an important constituent of aqueous fluids which are concentrated during the late-stage crystallization of igneous intrusive rocks. This is especially true of granitic and alkaline plutonic rocks which are initially much richer in fluorine than are basic intrusive rocks1. Either ...
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 203 (1964), S. 510-511 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A similar process for basic rocks, not previously recorded, is proposed for the basic hornfelses of the Land's End granite aureole, Cornwall. Although the process involves progressive desilication, it is not strictly analogous to that seen in pelitic hornfelses as the basic hornfelses have little ...
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  • 3
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    PANGAEA
    In:  Supplement to: Floyd, Peter A (1986): Geochemistry and provenance of basaltic clasts within volcaniclastic debris flows, East Mariana Basin, Deep Sea Drilling Project Site 585. In: Moberly, R; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 89, 449-458, https://doi.org/10.2973/dsdp.proc.89.115.1986
    Publication Date: 2023-05-12
    Description: Pebble-sized basaltic and glassy clasts were extracted from seamount-derived volcaniclastic debris flows and analyzed for various trace elements, including the rare earths, to determine their genetic relationships and provenance. All the clasts were originally derived from relatively shallow submarine lava flows prior to sedimentary reworking, and have undergone minor low-grade alteration. They are classified into three petrographic groups (A, B, and C) characterized by different phenocryst assemblages and variable abundances and ratios of incompatible elements. Group A (clast from Hole 585) is a hyaloclastite fragment which is olivine-normative and distinct from the other clasts, with incompatibleelement ratios characteristic of transitional or alkali basalts. Groups B and C (clasts from Hole 585A) are quartz-normative, variably plagioclase-clinopyroxene-olivine phyric tholeiites, all with essentially similar ratios of highly incompatible elements and patterns of enrichment in light rare earth elements (chrondrite-normalized). Variation within Groups B and C was governed by low-pressure fractionation of the observed phenocryst phases, whereas the most primitive compositions of each group may be related by variable partial melting of a common source. The clasts have intraplate chemical characteristics, although relative to oceanic hot-spot-related volcanics (e.g., Hawaiian tholeiites) they are marginally depleted in most incompatible elements. The source region was enriched in all incompatible elements, compared with a depleted mid-ocean-ridge basalt source.
    Keywords: Deep Sea Drilling Project; DSDP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
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    PANGAEA
    In:  Supplement to: Floyd, Peter A; Rowbotham, G (1986): Chemistry of primary and secondary phases in intraplate basalts and volcaniclastic sediments, Deep Sea Drilling Project Leg 89. In: Moberly, R; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 89, 459-470, https://doi.org/10.2973/dsdp.proc.89.116.1986
    Publication Date: 2023-05-12
    Description: Electron microprobe data are presented for clinopyroxenes, plagioclases, palagonites, smectites, celadonites, and zeolites in Hole 462A sheet-flow basalts and Site 585 volcaniclastic sediments. Glomerocrystic clinopyroxenes in Hole 462A are predominantly Ti-poor augites with minor fractionation to ferroaugites in rim portions. Quenched plumose clinopyroxenes show considerable variation from Ca-rich to Ca-poor augites, although all are characterized by being Tirich and Cr-poor relative to the glomerocrysts. Two differentiated series of Site 585 pyroxene compositions, calcic augite and diopside-salite, demonstrate the coexistence, in the vitric and lithic clasts, of tholeiitic and alkali basalt types, respectively. Plagioclase compositions in all samples are mainly labradorites, although some zoned Hole 462A glomerocrysts range from An73 to An20 and are characterized by high Mg and Fe contents in the more calcic varieties. The K content of the plagioclases is highest in the more sodic crystals, although the overall higher orthoclase component of Site 585 plagioclases reflects the generally higher bulk-rock K content. The compositions of both secondary smectites and celadonites are similar irrespective of the alteration location (glass, matrix, vesicles, etc.), although brown smectites replacing interstitial glass have marginally higher total Fe contents than pale green and yellow smectites. Analyzed zeolites are mainly phillipsites with variable alkali content, and, together with associated celadonite, represent late-stage alteration repositories for K under mildly oxidizing conditions. The compositions of both early and late secondary minerals are typical of those formed by the submarine alteration of basaltic rocks at low temperatures.
    Keywords: Deep Sea Drilling Project; DSDP
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Floyd, Peter A (1986): Glassy and basaltic fragments within graded volcaniclastic sediments, East Mariana Basin, Deep Sea Drilling Project Leg 89. In: Moberly, R; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 89, 433-447, https://doi.org/10.2973/dsdp.proc.89.114.1986
    Publication Date: 2023-06-27
    Description: Graded volcaniclastic sediments deposited by turbidity currents in the basal section at Site 585 are mixed vitric-lithic tuffs and lapilli-stones with minor Plagioclase and clinopyroxene crystal fragments. They represent the reworked products of basaltic hyaloclastite accumulations that developed on the flanks and tops of nearly emergent seamounts. They were subsequently swept to the abyssal depths of the southern Mariana Basin by turbitity currents, along with minor reef debris. Vesicles in glassy clasts are on average very small (0.1-0.2 mm diameter), although their volumes, as a percentage of the enclosing glass, are relatively high and suggest a maximum depth of initial lava intrusion of 〈 400 m. A shallow-water environment for the hyaloclastites is indicated by the commonly associated shallow-water faunal debris and ooids. There is no clear evidence of epiclastic or pyroclastic material associated with the hyaloclastites. Glass, rarely preserved as sideromelane, is generally replaced by palagonite or smectites, and ranges from highly vesicular aphyric to moderately vesicular phyric types, with various assemblages of olivine, Plagioclase, and clinopyroxene microphenocrysts and megaphenocrysts. Lithic clasts exhibit a range of textures—from opaque quench-textured tachylite glass to hypocrystalline and holocrystalline basalts—which are commonly Plagioclase- or plagioclase-clinopyroxene- phyric. Correlation of primary petrographic features between vitric and lithic clasts and textures, based on cooling history, allows the identification of five "lava types," each of which represents an extrusive episode. All the volcaniclastics are pervasively altered, with the development of palagonite, various colored smectites, celadonite, and zeolites typical of the lower zeolite facies. Two phases of alteration are recognized: submarine alteration after initial fragmentation, and subsequent alteration during burial after transportation to abyssal depths.
    Keywords: 89-585; 89-585A; Deep Sea Drilling Project; Diameter; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Leg89; Length; Length, standard deviation; Lithologic unit/sequence; Lithology/composition/facies; North Pacific/BASIN; Replicates; Sample code/label; Standard deviation; Volume
    Type: Dataset
    Format: text/tab-separated-values, 205 data points
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  • 6
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    PANGAEA
    Publication Date: 2023-06-27
    Keywords: 89-585; 89-585A; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Leg89; Lithologic unit/sequence; Lithology/composition/facies; North Pacific/BASIN; Petrography description; Sample, optional label/labor no; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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  • 7
    Publication Date: 2023-06-27
    Keywords: 89-585; 89-585A; Albite; Anorthite; Apatite; Deep Sea Drilling Project; Diopside; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Hypersthene; Ilmenite; Leg89; Magnetite; North Pacific/BASIN; Olivine; Orthoclase; Quartz; Sample, optional label/labor no; Sample code/label; Wollastonite
    Type: Dataset
    Format: text/tab-separated-values, 99 data points
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  • 8
    Publication Date: 2023-06-27
    Keywords: 89-462A; 89-585; 89-585A; Aluminium (IV); Aluminium (VI); Aluminium oxide; Calcium; Calcium oxide; Calculated based on oxygen number; Chromium; Chromium(III) oxide; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Event label; Glomar Challenger; Iron 2+ and 3+; Iron oxide, FeO; Leg89; Magnesium; Magnesium oxide; Manganese; Manganese oxide; North Pacific; North Pacific/BASIN; Potassium; Potassium oxide; Sample, optional label/labor no; Sample code/label; Sample comment; Silicon; Silicon dioxide; Sodium; Sodium oxide; Titanium; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 480 data points
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  • 9
    Publication Date: 2023-06-27
    Keywords: 89-462A; 89-585; 89-585A; Deep Sea Drilling Project; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Leg89; Lithologic unit/sequence; Lithology/composition/facies; North Pacific; North Pacific/BASIN; Sample, optional label/labor no; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 10
    Publication Date: 2023-06-27
    Keywords: 89-462A; 89-585; 89-585A; Aluminium; Aluminium oxide; Calcium; Calcium oxide; Calculated based on oxygen number; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Event label; Glomar Challenger; Iron 2+ and 3+; Iron oxide, FeO; Leg89; Magnesium; Magnesium oxide; Manganese; Manganese oxide; North Pacific; North Pacific/BASIN; Potassium; Potassium oxide; Sample, optional label/labor no; Sample code/label; Sample comment; Silicon; Silicon dioxide; Sodium; Sodium oxide; Titanium; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 420 data points
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