Search Constraints

Start Over
Filtering by: Creator Merritt, Patrick A. Remove constraint Creator: Merritt, Patrick A. Rights Statement Copyright Not Evaluated Remove constraint Rights Statement: Copyright Not Evaluated

Search Results

  • MCNP benchmarking and analysis of Oregon State University TRIGA Reactor

    Creator:
    Merritt, Patrick A.
    Resource Type:
    Masters Thesis
    Full Text:
    TRIGA Reactor AN ABSTRACT OF THE THESIS OF Patrick A. Merritt for the degree of Master of Science

  • Plate 8.jpg

    Creator:
    Jackson, Patrick A.
    Abstract:
    The Pleistocene Carpinteria basin is an east-trending northward-verging, faulted syncline containing up to 1220m of partially intertonguing Santa Barbara and Casitas Formations deposited on previously folded pre- Pleistocene strata with up to 80° discordance. Structures subcropping against the unconformity indicate most of the deformation in the Santa Ynez Range prior...

  • Plate 7.jpg

    Creator:
    Jackson, Patrick A.
    Abstract:
    The Pleistocene Carpinteria basin is an east-trending northward-verging, faulted syncline containing up to 1220m of partially intertonguing Santa Barbara and Casitas Formations deposited on previously folded pre- Pleistocene strata with up to 80° discordance. Structures subcropping against the unconformity indicate most of the deformation in the Santa Ynez Range prior...

  • Plate 6.jpg

    Creator:
    Jackson, Patrick A.
    Abstract:
    The Pleistocene Carpinteria basin is an east-trending northward-verging, faulted syncline containing up to 1220m of partially intertonguing Santa Barbara and Casitas Formations deposited on previously folded pre- Pleistocene strata with up to 80° discordance. Structures subcropping against the unconformity indicate most of the deformation in the Santa Ynez Range prior...

  • Plate 5.jpg

    Creator:
    Jackson, Patrick A.
    Abstract:
    The Pleistocene Carpinteria basin is an east-trending northward-verging, faulted syncline containing up to 1220m of partially intertonguing Santa Barbara and Casitas Formations deposited on previously folded pre- Pleistocene strata with up to 80° discordance. Structures subcropping against the unconformity indicate most of the deformation in the Santa Ynez Range prior...

  • Plate 4.jpg

    Creator:
    Jackson, Patrick A.
    Abstract:
    The Pleistocene Carpinteria basin is an east-trending northward-verging, faulted syncline containing up to 1220m of partially intertonguing Santa Barbara and Casitas Formations deposited on previously folded pre- Pleistocene strata with up to 80° discordance. Structures subcropping against the unconformity indicate most of the deformation in the Santa Ynez Range prior...

  • Plate 3.jpg

    Creator:
    Jackson, Patrick A.
    Abstract:
    The Pleistocene Carpinteria basin is an east-trending northward-verging, faulted syncline containing up to 1220m of partially intertonguing Santa Barbara and Casitas Formations deposited on previously folded pre- Pleistocene strata with up to 80° discordance. Structures subcropping against the unconformity indicate most of the deformation in the Santa Ynez Range prior...

  • Plate 2.jpg

    Creator:
    Jackson, Patrick A.
    Abstract:
    The Pleistocene Carpinteria basin is an east-trending northward-verging, faulted syncline containing up to 1220m of partially intertonguing Santa Barbara and Casitas Formations deposited on previously folded pre- Pleistocene strata with up to 80° discordance. Structures subcropping against the unconformity indicate most of the deformation in the Santa Ynez Range prior...

  • Plate 19.jpg

    Creator:
    Jackson, Patrick A.
    Abstract:
    The Pleistocene Carpinteria basin is an east-trending northward-verging, faulted syncline containing up to 1220m of partially intertonguing Santa Barbara and Casitas Formations deposited on previously folded pre- Pleistocene strata with up to 80° discordance. Structures subcropping against the unconformity indicate most of the deformation in the Santa Ynez Range prior...

  • Plate 1.jpg

    Creator:
    Jackson, Patrick A.
    Abstract:
    The Pleistocene Carpinteria basin is an east-trending northward-verging, faulted syncline containing up to 1220m of partially intertonguing Santa Barbara and Casitas Formations deposited on previously folded pre- Pleistocene strata with up to 80° discordance. Structures subcropping against the unconformity indicate most of the deformation in the Santa Ynez Range prior...