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Showing 1 to 20 of 115 for “"petrogenesis"”.

  1. Petrogenesis of the Eshowe melilitites

    The Eshowe melilitites intruded marginal cratonic crust at approximately 80my. Their intrusion followed after a long period of extensive rift tectonism associated with the breakup of Gondwanaland. The intrusives represent the final phase of alkaline and basaltic magmatism that commenced at about …

    cape-town Repository record for Petrogenesis of the Eshowe melilitites (opens in a new tab)

  2. Silicate Melt Inclusions in Igneous Petrogenesis

    Silicate melt inclusions are ubiquitous in quartz phenocrysts, yet there are few studies of such inclusions from porphyry copper systems. A melt inclusion forms when magma is trapped in a growing phenocryst. If a phenocryst is able to preserve the original parent magma, then accurate information …

    vt Repository record for Silicate Melt Inclusions in Igneous Petrogenesis (opens in a new tab)

  3. Petrogenesis of the Moosehorn igneous complex, Maine

    New radiometric ages and field relations within the Coastal Maine Magmatic Province suggest a bimodal distribution of igneous rocks in both space and time. The earlier magmatic event is represented by the development of large igneous complexes which occur along a magmatic axis extending from Calais …

    vt Repository record for Petrogenesis of the Moosehorn igneous complex, Maine (opens in a new tab)

  4. Petrogenesis of the Springfield Granodiorite, southeast Pennsylvania Piedmont

    The Springfield pluton intrudes the Wissahickon schist in the southeast Pennsylvania Piedmont. The mineralogy of the pluton. in order of decreasing abundance is plagioclase, quartz, microcline, biotite, epidote (often with allanite cores) and trace amounts of hornblende. Accessory minerals include …

    vt Repository record for Petrogenesis of the Springfield Granodiorite, southeast Pennsylvania Piedmont (opens in a new tab)

  5. Petrogenesis of the Spruce Pine pegmatites, North Carolina

    Pegmatites in the Spruce Pine district, North Carolina, are an example of muscovite class pegmatites that were derived from differentiation of a magma. There are eight granodiorite plutons in the Spruce Pine area ranging in size from 1 to 20 square kilometers that contain and are surrounded by …

    vt Repository record for Petrogenesis of the Spruce Pine pegmatites, North Carolina (opens in a new tab)

  6. Element fractionation in the petrogenesis of ocean island basalts

    Analytical techniques have been developed to measure the very small [230ThP32Th] atomic ratios (3-8x10-6) typical of basaltic lavas using a single focussing mass spectrometer. Compared to conventional alpha-counting methods, the technique presented typically gives a 2-5 fold improvement in …

    the-open-u Repository record for Element fractionation in the petrogenesis of ocean island basalts (opens in a new tab)

  7. The Origin and Petrogenesis of the Ethiopian Flood Basalts

    The volcanic rocks of the Afro-Arabian volcanic province chart the nature and evolution of the mantle plume source responsible for a major continental flood basalt event and the manner in which it interacted with the lithosphere over the course of continental separation. The flood basalts of the …

    the-open-u Repository record for The Origin and Petrogenesis of the Ethiopian Flood Basalts (opens in a new tab)

  8. Trace element zoning in garnets--implications for metamorphic petrogenesis

    Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric and Planetary Sciences, 1988.

    mit Repository record for Trace element zoning in garnets--implications for metamorphic petrogenesis (opens in a new tab)

  9. Petrogenesis of the reversely zoned Turtle pluton, Southeastern California

    Few plutons with a reversed geometry of a felsic rim and mafic core have been described in the geologic literature. The Turtle pluton of S.E. California is an intrusion composed of a granitic rim and granodioritic core and common microgranitoid enclaves. Field observations, mineral textures, and …

    vt Repository record for Petrogenesis of the reversely zoned Turtle pluton, Southeastern California (opens in a new tab)

  10. Applications of Melt Inclusions to Problems in Igneous Petrogenesis

    … and field studies to better understand igneous petrogenesis. One potential problem associated with melt inclusions is water-loss during laboratory heating. A Raman spectroscopic technique was developed to determine water contents of silicate glasses, and this technique was applied to monitor …

    vt Repository record for Applications of Melt Inclusions to Problems in Igneous Petrogenesis (opens in a new tab)

  11. Petrogenesis and thermal history of the Kunlun Batholith, Northern Tibet

    The Kunlun Terrane is the most northerly of the several microplates that comprise the Tibetan Plateau. Geochronological data from the Kunlun batholith defines three distinct periods of intrusion at 390 Ma, 250 Ma and 190 Ma. A model is presented whereby the Devonian intrusions are considered to be …

    the-open-u Repository record for Petrogenesis and thermal history of the Kunlun Batholith, Northern Tibet (opens in a new tab)

  12. Petrogenesis of crustal xenoliths from San Carlos Indian Reservation, Arizona

    Includes bibliographical references (pages 165-173).

    colo-mines Repository record for Petrogenesis of crustal xenoliths from San Carlos Indian Reservation, Arizona (opens in a new tab)

  13. The petrogenesis of Liberian diamondiferous rocks, Man Craton, West Africa

    Kimberlites and lamproites are ultramafic igneous rocks believed to originate from the convective asthenosphere and sub-continental lithospheric mantle, respectively, however, the genetic link between these rock types is still a debate among researchers. Recently, it has been shown (e.g., in the …

    cape-town Repository record for The petrogenesis of Liberian diamondiferous rocks, Man Craton, West Africa (opens in a new tab)

  14. Petrogenesis of a migmatite, Penobscot County, Maine: ultrametamorphism or intrusion?

    The Clifton Migmatite crops out between the biotite grade Bucksport Formation (predominantly calcareous pelitic quartzite) on the west, the Lucerne Pluton (biotite granite) on the southeast, and the Parks Pond Pluton (mafic granite to quartz syenite) on the northeast. The Parks Pond crystallized at …

    vt Repository record for Petrogenesis of a migmatite, Penobscot County, Maine: ultrametamorphism or intrusion? (opens in a new tab)

  15. Geochemistry and petrogenesis of the Catoctin Volcanic Province, central Appalachians

    The Catoctin Volcanic Province represents a sequence of rift related tholeiitic magmas erupted during late Precambrian opening of the Iapetus ocean basin. Three transects have been mapped across the province in northern Virginia in order to demonstrate that there is a mappable stratigraphy and to …

    vt Repository record for Geochemistry and petrogenesis of the Catoctin Volcanic Province, central Appalachians (opens in a new tab)

  16. Basalt petrogenesis beneath slow- and ultraslow-spreading Arctic mid-ocean ridges

    To explore the ability of melting mafic lithologies to produce alkaline ocean-island basalts (OIB), an experimental study was carried out measuring clinopyroxene (Cpx)- melt and garnet (Gt)-melt partition coefficients during silica-poor garnet pyroxenite melting for a suite of trace elements, …

    woods-hole Repository record for Basalt petrogenesis beneath slow- and ultraslow-spreading Arctic mid-ocean ridges (opens in a new tab)

  17. Stratigraphy and petrogenesis of the Parana continental flood basalts, southern Brazil

    The Early Cretaceous (~130 Ma) Paraná lavas of South America represent the largest preserved example of a continental flood basalt (CFB) province, with a present area in excess of 1.2 x 10<sup>6</sup> km<sup>2</sup>. Magmatism is dominated by tholeiitic basalts (> 90 %), with minor rhyolites as a …

    the-open-u Repository record for Stratigraphy and petrogenesis of the Parana continental flood basalts, southern Brazil (opens in a new tab)

  18. Geochemistry and petrogenesis of the Proterozoic Pater metavolcanic suite, Spragge, Ontario /

    The Pater metavolcanic suite (PVS) was extruded as part O'f the basal Pater Formation of the Huronian Supergroup ca. 2.4 Ga. They Ars classified as wi thin-plate tholeiites associated with an immature ri-fting episode, and are inter layered with associated vol cani clastic and metasedimentary …

    brock Repository record for Geochemistry and petrogenesis of the Proterozoic Pater metavolcanic suite, Spragge, Ontario / (opens in a new tab)

  19. Petrogenesis of the False Bay dyke swarm, Cape Peninsula, South Africa

    The False Bay dyke swarm is the southern-most set of Early Cretaceous dolerite dyke intrusions along the western margin of southern Africa associated with rifting of Gondwana and opening of the South Atlantic Ocean. Previous work highlighted the evolution of a single magma type from …

    cape-town Repository record for Petrogenesis of the False Bay dyke swarm, Cape Peninsula, South Africa (opens in a new tab)

  20. Petrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africa

    The Outoitspan Group 1 kimberlite pipe forms part of the well-known cluster of pipes located in and around the city of Kimberley, South Africa. Eight macroscopically distinct intrusive phases, i.e. D2 Type 2, D2 Type 3, D2/D5, D5, D18, Type 5, D16 and the D16 dyke are present in the Northwest …

    cape-town Repository record for Petrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africa (opens in a new tab)

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