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  • 1
    Unknown
    New Views of the Moon (2006)
    Chantilly, Va. : Mineralogical Society of America
    Details
    Description / Table of Contents: The very successful orbital missions of the 1990's, Clementine and Lunar Prospector, provided key mineralogical, geochemical, and geophysical data sets that extended our view of the Moon beyond what we knew from Apollo and Luna exploration to a truly global perspective. These new data sets have been integrated with information gained from three preceding decades of study of lunar samples and older, less complete remotely sensed data sets. Although there have been no new lunar sample-return missions since Apollo and Luna, new samples are available in the form of meteorites, recognized to be pieces of the Moon. These, too, play a role in improved knowledge of the Moon and in helping to couple information obtained by remote sensing with information obtained from rock and soil samples. As we stand on the edge of a new era of lunar and planetary exploration, including new missions to the Moon, Mars, and other planets and moons, we find it essential to examine in depth how the wide variety of data sets obtained during the course of lunar exploration can be used together to better understand the formation of the Moon and how it evolved to its present state. Such an understanding holds important lessons for the new era of lunar exploration as well as the exploration of other planets in the Solar System. This will ultimately lead to better knowledge of how our own planet Earth - with its unique environment suitable for the origin and evolution of life - originated and changed with time. This book assesses the current state of knowledge of lunar geoscience, given the data sets provided by missions of the 1990's, and lists remaining key questions as well as new ones for future exploration to address. It documents how a planet or moon other than the world on which we live can be studied and understood in light of integrated suites of specific kinds of information. The Moon is the only body other than Earth for which we have material samples of known geologic context for study. This book seeks to show how the different kinds of information gained about the Moon relate to each other and also to learn from this experience, thus allowing more efficient planning for the exploration of other worlds.
    Pages: Online-Ressource (XXII, 772 Seiten)
    ISBN: 0939950723
    URL: http://rimg.geoscienceworld.org/content/60/1.toc
    Language: English
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    E-BOOK
  • 2
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    Geochemistry of ODP Hole 183-1137A basalts (2009)
    PANGAEA
    In:  Supplement to: Kinman, William S; Neal, Clive R; Davidson, Jon P; Font, Laura (2009): The dynamics of Kerguelen Plateau magma evolution: New insights from major element, trace element and Sr isotope microanalysis of plagioclase hosted in Elan Bank basalts. Chemical Geology, 264(1-4), 247-265, https://doi.org/10.1016/j.chemgeo.2009.03.010
    Details
    Publication Date: 2024-01-09
    Description: The Kerguelen Plateau and Broken Ridge in the southern Indian Ocean together represent one of the most voluminous large igneous provinces (LIPs) ever emplaced on Earth. A scientific objective of Ocean Drilling Program (ODP) Leg 183 was to constrain the post-melting magma evolution of Kerguelen Plateau magmas. In an effort to better understand this evolution, isotopic and trace element analysis of individual plagioclase crystals hosted within two Kerguelen Plateau basalts recovered from Elan Bank were undertaken. Previous whole-rock studies established that the two host basalts investigated in this study are samples of crustally contaminated (lower group) and relatively uncontaminated (upper group) basalt. Plagioclase phenocrysts from the uncontaminated basalt are dominantly normal zoned and exhibit a 87Sr/86SrI range of 0.704845-0.704985, which overlaps uncontaminated group whole-rock values previously reported. Plagioclase crystals from the contaminated basalt are dominantly reverse zoned and exhibit a 87Sr/86SrI range of 0.705510-0.705735, which all lie within contaminated group whole-rock values previously reported. There are no systematic within crystal core to rim variations in 87Sr/86SrI from either group, with the exception that contaminated group crystal rims have overall less radiogenic 87Sr/86SrI than other zones. These observations indicate that crustal assimilation occurred before the formation of Unit 10 plagioclase phenocrysts, which is supported by parent magma trace element abundance data inverted using carefully calculated partition coefficients. Trace element diffusion modeling indicates that the upper group basalt (Unit 4) experienced a more vigorous eruptive flux than the lower group basalt (Unit 10). We suggest that plagioclase phenocrysts in both the upper and lower group basalts originated from the shallowest section of what was likely a complex magma chamber system. We contend that the magmatic system contained regions of extensive plagioclase-dominated crystal mush. Crustal assimilation was not a significant ongoing process in this portion of the Elan Bank magmatic system. Both basalts exhibit compelling evidence for remobilization and partial resorption of crystalline debris (e.g., reverse zoned crystals, glomerocrysts). We suggest Unit 4 and 10 magmas ascended different sections of the Elan Bank magma system, where the Unit 10 magmas ascended a section of the magma system that penetrated a stranded fragment of continental crust.
    Keywords: 183-1137A; DRILL; Drilling/drill rig; Indian Ocean; Joides Resolution; Leg183; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 3
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    (Table S1) Age determination of Emperor Seamounts basement (2003)
    PANGAEA
    In:  Supplement to: Tarduno, John A; Duncan, Robert A; Scholl, David W; Cottrell, Rory D; Steinberger, Bernhard; Thordarson, Thorvaldur; Kerr, Bryan C; Neal, Clive R; Frey, Frederick A; Torii, Masayuki; Carvallo, Claire (2003): The Emperor Seamounts: Southward motion of the Hawaiian hotspot plume in earth's mantle. Science, 301(5636), 1064-1069, https://doi.org/10.1126/science.1086442
    Details
    Publication Date: 2024-01-09
    Description: The Hawaiian-Emperor hotspot track has a prominent bend, which has served as the basis for the theory that the Hawaiian hotspot, fixed in the deep mantle, traced a change in plate motion. However, paleomagnetic and radiometric age data from samples recovered by ocean drilling define an age-progressive paleolatitude history, indicating that the Emperor Seamount trend was principally formed by the rapid motion (over 40 millimeters per year) of the Hawaiian hotspot plume during Late Cretaceous to early-Tertiary times (81 to 47 million years ago). Evidence for motion of the Hawaiian plume affects models of mantle convection and plate tectonics, changing our understanding of terrestrial dynamics.
    Keywords: 19-192; 197-1203A; 197-1204B; 197-1205A; 197-1206A; Age, 40Ar/39Ar Argon-Argon; Age, dated; Age, dated standard deviation; Argon-40/Argon-36; Argon-40/Argon-36, standard deviation; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Joides Resolution; Leg19; Leg197; North Pacific/GUYOT; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Sample comment
    Type: Dataset
    Format: text/tab-separated-values, 222 data points
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  • 4
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    (Table 1) Geochemistry of plagioclase of ODP Hole 183-1137A Unit 4 basalts (2009)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 183-1137A; Aluminium oxide; Anorthite; Barium; Calcium oxide; Cerium; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Elements, total; Europium; Indian Ocean; Iron oxide, FeO; Joides Resolution; LA-ICP-MS, Laser-ablation inductively coupled plasma mass spectrometer; Lanthanum; Lead; Leg183; Magnesium oxide; Neodymium; Ocean Drilling Program; ODP; Phosphorus pentoxide; Potassium oxide; Praseodymium; Rubidium; Samarium; Sample code/label; Sample code/label 2; Sample comment; Scandium; Silicon dioxide; Sodium oxide; Strontium; Titanium; Titanium dioxide; Vanadium; Yttrium
    Type: Dataset
    Format: text/tab-separated-values, 834 data points
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  • 5
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    (Table 3) Strontium isotope ratios of plagioclase of ODP Hole 183-1137A basalts (2009)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 183-1137A; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Indian Ocean; Joides Resolution; LA-ICP-MS, Laser-ablation inductively coupled plasma mass spectrometer; Leg183; Ocean Drilling Program; ODP; Rubidium/Strontium ratio; Sample code/label; Sample code/label 2; Sample comment; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error
    Type: Dataset
    Format: text/tab-separated-values, 136 data points
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  • 6
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    (Table 1) Platinum-group, major, and trace element abundances in ODP Hole 183-1136A basalts (2005)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 183-1136A; Barium; Caesium; Calculated; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Gadolinium; Hafnium; Holmium; Indian Ocean; Inductively coupled plasma - mass spectrometry (ICP-MS); Iridium; Iron oxide, Fe2O3; Joides Resolution; Lanthanum; Lead; Leg183; Lithologic unit/sequence; Lutetium; Magnesium oxide; Neodymium; Nickel; Niobium; Ocean Drilling Program; ODP; Palladium; Piece; Platinum; Praseodymium; Rhodium; Rock type; Rubidium; Ruthenium; Samarium; Sample code/label; Scandium; Strontium; Tantalum; Terbium; Thorium; Thulium; Titanium dioxide; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 100 data points
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  • 7
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    (Table 1) Platinum-group, major, and trace element abundances in ODP Hole 183-1137A basalts (2005)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 183-1137A; Barium; Caesium; Calculated; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Gadolinium; Hafnium; Holmium; Indian Ocean; Inductively coupled plasma - mass spectrometry (ICP-MS); Iridium; Joides Resolution; Lanthanum; Lead; Leg183; Lithologic unit/sequence; Lutetium; Neodymium; Nickel; Niobium; Ocean Drilling Program; ODP; Palladium; Piece; Platinum; Praseodymium; Rhodium; Rock type; Rubidium; Ruthenium; Samarium; Sample code/label; Scandium; Strontium; Tantalum; Terbium; Thorium; Thulium; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 8
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    (Table 1) Platinum-group, major, and trace element abundances in ODP Hole 183-1138A basalts (2005)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 183-1138A; Barium; Caesium; Calculated; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Gadolinium; Hafnium; Holmium; Indian Ocean; Inductively coupled plasma - mass spectrometry (ICP-MS); Iridium; Iron oxide, Fe2O3; Joides Resolution; Lanthanum; Lead; Leg183; Lithologic unit/sequence; Lutetium; Magnesium oxide; Neodymium; Nickel; Niobium; Ocean Drilling Program; ODP; Palladium; Piece; Platinum; Praseodymium; Rhodium; Rock type; Rubidium; Ruthenium; Samarium; Sample code/label; Scandium; Strontium; Tantalum; Terbium; Thorium; Thulium; Titanium dioxide; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 448 data points
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  • 9
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    Unknown
    (Table 1) Platinum-group, major, and trace element abundances in ODP Hole 183-1141A basalts (2005)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 183-1141A; Barium; Caesium; Calculated; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Gadolinium; Hafnium; Holmium; Indian Ocean; Inductively coupled plasma - mass spectrometry (ICP-MS); Iridium; Iron oxide, Fe2O3; Joides Resolution; Lanthanum; Lead; Leg183; Lithologic unit/sequence; Lutetium; Magnesium oxide; Neodymium; Nickel; Niobium; Ocean Drilling Program; ODP; Palladium; Piece; Platinum; Praseodymium; Rhodium; Rock type; Rubidium; Ruthenium; Samarium; Sample code/label; Scandium; Strontium; Tantalum; Terbium; Thorium; Thulium; Titanium dioxide; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 100 data points
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  • 10
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    (Table 1) Platinum-group, major, and trace element abundances in ODP Hole 183-1142A basalts (2005)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 183-1142A; Barium; Caesium; Calculated; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Gadolinium; Hafnium; Holmium; Indian Ocean; Inductively coupled plasma - mass spectrometry (ICP-MS); Iridium; Iron oxide, Fe2O3; Joides Resolution; Lanthanum; Lead; Leg183; Lithologic unit/sequence; Lutetium; Magnesium oxide; Neodymium; Nickel; Niobium; Ocean Drilling Program; ODP; Palladium; Piece; Platinum; Praseodymium; Rhodium; Rock type; Rubidium; Ruthenium; Samarium; Sample code/label; Scandium; Strontium; Tantalum; Terbium; Thorium; Thulium; Titanium dioxide; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 100 data points
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