Showing 32,781 - 32,800 results of 34,042 for search '"Rock On!!"', query time: 0.23s Refine Results
  1. 32781

    PETROGENESA DAN POTENSI MINERALISASI PADA GRANIT ANGGI, KABUPATEN MANOKWARI, PROVINSI PAPUA BARAT by , JUMIKO NOMPI SARIRA, , Dr. Lucas Donny Setijadji, S.T., M.Sc

    Published 2014
    “…The purpose of this research was to determine the petrographic and geochemical characteristics of the rocks and is expected to provide a good information and knowledge about the petrogenesis formation on the Anggi Granite. …”
    Thesis
  2. 32782

    ANALISIS KEKUATAN DINDING BATAKO DENGAN BALOK-KOLOM PRECAST DAN PRESTRESSED AKIBAT BEBAN STATIK by , AJENG ROSPRATAMI, , Arief Setiawan Budi Nugroho, ST., M.Eng., Ph.D.

    Published 2014
    “…From the pattern of cracking that occurs during testing, the collapse that occurred in the test object can be classified into Rocking Failure Mode (failure bolsters). Based on the test results, the stiffness value of the yield condition of DBP is higher than DBTP.…”
    Thesis
  3. 32783

    PENCEMARAN NITRAT DI AIRTANAH KECAMATAN GAMPING, KABUPATEN SLEMAN, DIY by , YOGA PURBAYA A.W, , Dr. Wahyu Wilopo, S.T., M.Eng.

    Published 2014
    “…Type of aquifer affect on permeability and porosity values, where the rocks that making up the porous and large fractures aquifers tend to have low nitrate concentrations, because of groundwater into the aquifer just passed involuntarily. …”
    Thesis
  4. 32784

    ANALISIS KEKUATAN DINDING MORTAR COR DI TEMPAT DENGAN PERKUATAN TULANGAN HORIZONTAL DAN BALOK-KOLOM PRECAST AKIBAT BEBAN STATIK by , KRISTIAN TRI ANGGORO, , Arief Setiawan Budi Nugroho, ST., M.Eng., Ph.D.

    Published 2014
    “…The result is that the damage type in mortar wall with horizontal reinforcement and concrete brick wall is rocking failure. The lateral load capacity of mortal wall in yield condition is 26.57 kN, it has 20.99% higher than concrete brick wall which has value of 21.96 kN. …”
    Thesis
  5. 32785

    REDISTRIBUSI KARBON ORGANIK TANAH (C-ORGANIK) MELALUI MEKANISME LONGSORLAHAN DI DAS KAYANGAN KABUPATEN KULON PROGO DAERAH ISTIMEWA YOGYAKARTA by , Nur Indah Sari Dewi, , Dr. Danang Sri hadmoko, M. Sc.

    Published 2012
    “…The research findings as follow: Type of landslide occur in Kayangan catchment is slide type which consists of the constituent material rocks and thin soil horizon with the arrangement of A and C, and forms a convex slope, it makes the slope unstable. …”
    Thesis
  6. 32786

    KAJIAN POTENSI OBYEK DAYA TARIK WISATA DAN PENINGKATAN PERANSERTA MASYARAKAT DALAM KONSEP KEPARIWISATAAN ALAM BERBASIS MASYARAKAT (Community Based Tourism) DI PANTAI WISATA DISA... by DJALAL, ABDURRAHMAN

    Published 2012
    “…This beach is very interested to visit because it has natural attraction that becomes main potency especially the beauty of the beach and the rocks along the beach. The geographic spatial which is close to the city centre makes Disa beach becoming the most wanted place to visit. …”
    Thesis
  7. 32787

    Ductile shear zones beneath strike-slip faults: Implications for the thermomechanics of the San Andreas fault zone by Thatcher, W, England, P

    Published 1998
    “…The fluid has the (linearized) conventional rheology assumed to apply to lower crust/upper mantle rocks. The temperature dependence of the effective viscosity of the fluid and the shear heating that accompanies deformation have been incorporated into the calculations, as has thermal conduction in an overlying crustal layer. …”
    Journal article
  8. 32788

    Viscous anisotropy of textured olivine aggregates, Part 2: Micromechanical model by Hansen, L, Conrad, C, Boneh, Y, Skemer, P, Warren, J, Kohlstedt, D

    Published 2016
    “…<p>The significant viscous anisotropy that results from crystallographic alignment (texture) of olivine grains in deformed upper-mantle rocks strongly influences a large variety of geodynamic processes. …”
    Journal article
  9. 32789

    Timing of metamorphism of the Lansang gneiss and implications for left-lateral motion along the Mae Ping (Wang Chao) strike-slip fault, Thailand by Palin, R, Searle, M, Morley, C, Charusiri, P, Horstwood, M, Roberts, N

    Published 2013
    “…This age is interpreted to date the timing of dyke emplacement, implying that the MPF cuts through earlier formed magmatic and high-grade metamorphic rocks. These new data, when combined with regional mapping and earlier geochronological work, show that neither metamorphism, nor regional cooling, was directly related to strike-slip motion. © 2013 Elsevier Ltd.…”
    Journal article
  10. 32790

    Plate tectonics: what, where, why, and when? by Palin, RM, Santosh, M

    Published 2020
    “…A transitional period during the Neoarchean and Paleoproterozoic/Mesoproterozoic was characterized by continued secular cooling of the Earth's mantle, which reduced the buoyancy of oceanic lithosphere and increased its strength, allowing the angle of subduction at convergent plate margins to gradually steepen. The appearance of rocks during the Neoproterozoic (c. 0.8&#x2013;0.9 Ga) diagnostic of subduction do not mark the onset of plate tectonics, but simply record the beginning of modern-style cold, deep, and steep subduction that is an end-member state of an earlier, hotter, mobile lid regime.…”
    Journal article
  11. 32791

    An 11 Earth-mass, long-period Sub-Neptune orbiting a Sun-like star by Mayo, AW, Rajpaul, VM, Buchhave, LA, Dressing, CD, Mortier, A, Zeng, L, Fortenbach, CD, Aigrain, S, Bonomo, AS, Cameron, AC, Charbonneau, D, Coffinet, A, Cosentino, R, Damasso, M, Dumusque, X, Fiorenzano, AFM, Haywood, RD, Latham, DW, López-Morales, M, Malavolta, L, Micela, G, Molinari, E, Pearce, L, Pepe, F, Phillips, D, Poretti, E, Piotto, G, Rice, K, Sozzetti, A, Udry, S

    Published 2019
    “…The planet likely consists of a significant fraction of ices (dominated by water ice), in addition to rocks/metals, and a small amount of gas. Sophisticated modeling techniques such as those used in this paper, combined with future spectrographs with ultra high-precision and stability will be vital for yielding more mass measurements in this poorly understood exoplanet regime. …”
    Journal article
  12. 32792

    Experimental constraints on major and trace element partitioning during partial melting of eclogite by Klemme, S, Blundy, J, Wood, B

    Published 2002
    “…The data also indicate slight Nb/Ta fractionation during partial melting of bimineralic eclogite, which is not, however, sufficient to explain some recently observed Nb/Ta fractionation in island arc rocks. Accessory rutile, however, can explain such fractionation. …”
    Journal article
  13. 32793

    Theropod fauna from southern Australia indicates high polar diversity and climate-driven dinosaur provinciality by Benson, R, Rich, T, Vickers-Rich, P, Hall, M

    Published 2012
    “…We describe and review theropod dinosaur postcranial remains from the Aptian–Albian Otway and Strzelecki groups, based on at least 37 isolated bones, and more than 90 teeth from the Flat Rocks locality. Several specimens of medium- and large-bodied individuals (estimated up to ∼8.5 metres long) represent allosauroids. …”
    Journal article
  14. 32794

    Crustal melt granites and migmatites along the Himalaya: melt source, segregation, transport and granite emplacement mechanisms by Searle, M, Cottle, J, Streule, M, Waters, D

    Published 2009
    “…Melting was induced through a combination of thermal relaxation due to crustal thickening and from high internal heat production rates within the Proterozoic source rocks in the middle crust. Himalayan granites have highly radiogenic Pb isotopes and extremely high uranium concentrations. …”
    Journal article
  15. 32795

    Emergence of a habitable planet by Zahnle, K, Arndt, N, Cockell, C, Halliday, A, Nisbet, E, Selsis, F, Sleep, N

    Published 2007
    “…Recycling and distillation of hydrous basalts produced granitic rocks very early, which is consistent with preserved &gt;4 Ga detrital zircons. …”
    Journal article
  16. 32796

    Subduction-obduction related petrogenetic and metamorphic evolution of the Semail ophiolite sole in Oman and the United Arab Emirates by Cox, J, Jon S. Cox

    Published 2000
    “…Structural field observations, combined with petrological, isotopic and geochemical analysis of metamorphic and igneous rocks associated with the Semail ophiolite of Oman and the United Arab Emirates, have been used in conjunction with geochronology and estimates of metamorphic conditions and PT paths to constrain the ophiolite emplacement history. …”
    Thesis
  17. 32797

    The sedimentology, mineralogy and geochemistry of the ~1.4 ga Roper Superbasin Northern Australia by Johnson, B

    Published 2021
    “…</p> <p>To test these two hypotheses, I conducted a high-resolution study of exquisitely preserved ~1.4 - 1.3 Ga sedimentary rocks from the Roper Superbasin (RSB), northern Australia. …”
    Thesis
  18. 32798

    Dating blueschist-facies metamorphism within the Naga ophiolite, Northeast India, using sheared carbonate veins by Maibam, B, Palin, RM, Gerdes, A, White, RW, Foley, S

    Published 2022
    “…The tectonic significance of blueschist-facies rocks associated with the Indo-Myanmar ophiolite belt is uncertain, given the lack of detailed petrological study and the paucity of reliable age data for different stages in their geological evolution. …”
    Journal article
  19. 32799

    Extensional and compressional faults in the Everest–Lhotse massif, Khumbu Himalaya, Nepal

    Published 1999
    “…Both the normal faults at the top of the slab and the Khumbu thrust at the base of the leucogranite sheets were mechanically linked, resulting in the southward extrusion of rocks formed at c. 12–30 km depth within the High Himalayan slab. …”
    Journal article
  20. 32800

    Upper crustal structure of an active volcano from refraction/reflection tomography, Montserrat, Lesser Antilles by Paulatto, M, Minshull, T, Baptie, B, Dean, S, Hammond, J, Henstock, T, Kenedi, C, Kiddle, E, Malin, P, Peirce, C, Ryan, G, Shalev, E, Sparks, R, Voight, B

    Published 2010
    “…The upper crust beneath this reflector has velocities of 4.0-6.0 km s-1 and is inferred to correspond to plutonic and hypabyssal rocks and sedimentary material of the old arc. The high velocity region beneath the island, extends into the crust to a depth of at least 5 km, and is believed to be caused by an intrusive complex, possibly of intermediate composition. …”
    Journal article