Zobrazeno 1 - 10
of 11
pro vyhledávání: '"M. T. Heizler"'
Publikováno v:
Mineralogy and Petrology. 79:3-31
¶The Campanian Plain is an 80 × 30 km region of southern Italy, bordered by the Apennine Chain, that has experienced subsidence during the Quaternary. This region, volcanologically active in the last 600 ka, has been identified as the Campanian Vol
Publikováno v:
New Mexico Geological Society Annual Spring Meeting.
Publikováno v:
New Mexico Geological Society Annual Spring Meeting.
Autor:
K. E. Karlstrom, A. Darling, L. J. Crossey, R. Crow, D. Coblentz, W. Oiumet, E. Kirby, J. Van Wikk, B. Schmandt, S. A. Kelley, M. T. Heizler, R. Aster, J. MacCarthy, G. Lazear, A. Aslam, K. Dueker, J. Hansen, J. Stachnik
Publikováno v:
New Mexico Geological Society Annual Spring Meeting.
Publikováno v:
New Mexico Geological Society Annual Spring Meeting.
Publikováno v:
New Mexico Geological Society Annual Spring Meeting.
Autor:
John W. Delano, S. E. De Long, William S.F. Kidd, Carsten Schirnick, G. W. Putman, M. Ohr, M. T. Heizler, B. Bock
Publikováno v:
The Journal of Geology. 98:157-170
Altered volcanic ashes (K-bentonites) in the late Ordovician (Caradocian) Utica shale of New York State are the product of explosive arc volcanism. Most of the 30 K-bentonites examined in this investigation contain fragmental crystals and rock fragme
Autor:
J. M. Amato, A. O. Boullion, A. E. Sanders, G. Gehrels, M. T. Heizler, G. L. Farmer, L. C. Andronicos
Publikováno v:
New Mexico Geological Society, 2006 Annual Spring Meeting, Proceedings Volume.
Autor:
M. T. Heizler
Publikováno v:
New Mexico Geological Society, 2006 Annual Spring Meeting, Proceedings Volume.
Publikováno v:
Albuquerque Geology.