Výsledky vyhledávání - "David N. Shirley"

DISCOM2: Distance Computing the SP2 Pilot FY98 Report

Autor: David N. Shirley, John P. Noe, Walter H. VanDevender, Thomas J. Pratt, Sue P. Goudy, Judy Beiriger, Martha J. Ernest, David P. Wiltzius, Rupert K. Byers, Thomas D. Tarman

As a way to bootstrap the DISCOM(2) Distance Computing Program the SP2 Pilot Project was launched in March 1998. The Pilot was directed towards creating an environment to allow Sandia users to run their applications on the Accelerated Strategic Compu

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c63108f1ce5654596e587015835fd593
https://doi.org/10.2172/7018

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Differentiation and Compaction in the Palisades Sill, New Jersey

Autor: David N. Shirley

Publikováno v: Journal of Petrology. 28:835-865

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c1117e1f638cffa9eca2dd29f896d632
https://doi.org/10.1093/petrology/28.5.835

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Compaction of Igneous Cumulates

Autor: David N. Shirley

Publikováno v: The Journal of Geology. 94:795-809

When initially deposited, mafic igneous cumulates consist of a solid matrix of mineral phases plus 50-60% interstitial liquid. Due to its greater density the matrix compacts, squeezing the interstitial liquid upward. A numerical fluid mechanical mode

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::2d3c14c54d5324a1f1b14d908cf85d66
https://doi.org/10.1086/629088

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Petrology and chemistry of two 'large' granite clasts from the moon

Autor: Klaus Keil, David N. Shirley, John T. Wasson, G. Jeffrey Taylor, Paul H. Warren

Publikováno v: Earth and Planetary Science Letters. 64:175-185

Pristine granite clasts in Apollo-14 breccias 14321 and 14303 have estimated masses of 1.8 and 0.17 g, respectively. The 14321 clast is about 60 percent K-feldspar and 40 percent quartz, with traces of extremely Mg-poor mafic silicates and ilmenite.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6184e93b1ef4cdacea8155d79c9e894d
https://doi.org/10.1016/0012-821x(83)90202-9

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A potpourri of pristine Moon rocks, including a VHK mare basalt and a unique, augite-rich Apollo 17 anorthosite

Autor: Gregory W. Kallemeyn, Paul H. Warren, David N. Shirley

Publikováno v: Journal of Geophysical Research: Solid Earth. 91:319-330

The anorthosite fragment, 76504,18, the first of the Apollo 17's pristine anorthosites, was found to have: (1) a higher ratio of high-Ca pyroxine to low-Ca pyroxene, (2) higher Na in its plagioclase, (3) higher contents of incompatible elements, and

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::287d0458c0b1c19d7f8a78ff775358ac
https://doi.org/10.1029/jb091ib04p0d319

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SEVENTH FORAY: WHITLOCKITE-RICH LITHOLOGIES, A DIOPSIDE-BEARING TROCTOLITIC ANORTHOSITE, FERROAN ANORTHOSITES, AND KREEP

Autor: John T. Wasson, Paul H. Warren, Gregory W. Kallemeyn, Klaus Keil, David N. Shirley, G. Jeffrey Taylor

Publikováno v: Scopus-Elsevier

Seventeen nonmare samples, most of them pristine, are characterized, and implications of the new data are discussed. Five pristine samples are from Apollo 14, near the center of the KREEP-rich zone in the moon's western hemisphere. Three of them are

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fd4b4518a362b901bfc58732024190f4
http://www.scopus.com/inward/record.url?eid=2-s2.0-0020847761&partnerID=MN8TOARS

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A partially molten magma ocean model

Autor: David N. Shirley

Publikováno v: Journal of Geophysical Research. 88:A519

Under the assumption that the outer 300-400 km of the moon was at first only partially, rather than fully molten, an explanation of the properties of the lunar crust and upper mantle is obtained according to which nuclei of anorthositic crust formed

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::67396a5a2337c8c8dc787f7f607db799
https://doi.org/10.1029/jb088is02p0a519

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Correction to 'A potpourri of pristine Moon rocks, including a VHK mare basalt and a unique, augite-rich Apollo 17 anorthosite' by Paul H. Warren, David N. Shirley, and Gregory W. Kallemeyn

Autor: Gregory W. Kallemeyn, Paul H. Warren, David N. Shirley

Publikováno v: Journal of Geophysical Research: Solid Earth. 92:E775-E775

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::ee2b5e88a4c6614b4c33ab63a11f3ed6
https://doi.org/10.1029/jb092ib04p0e775

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