Zobrazeno 1 - 10
of 207
pro vyhledávání: '"C, Halls"'
Publikováno v:
Mineral Deposits at the Beginning of the 21st Century ISBN: 9781003077503
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c597bca3b4cba585ecdd2b54e6ee539
https://doi.org/10.1201/9781003077503-92
https://doi.org/10.1201/9781003077503-92
Autor:
Kevin R. Kosola, Frank G. Dohleman, Steven C. Halls, Michael A. Hall, Kevin C. Glenn, Elena A. Rice, Mohamed Bedair, Dmitry Grapov, Shilpa Swarup, Lex E. Flagel, Ryan A. Rapp, Sean Yang, Edwards M. Allen, Sarah L. Tucker, Kimberly M. Wegener
Publikováno v:
Plant, Cell & Environment. 43:880-902
A challenge to improve an integrative phenotype, like yield, is the interaction between the broad range of possible molecular and physiological traits that contribute to yield and the multitude of potential environmental conditions in which they are
Autor:
Giday WoldeGabriel, Nicholas J. G. Pearce, Henry C. Halls, John A. Westgate, René W. Barendregt, Michael P. Gorton, Andrei M. Sarna-Wojcicki, Emily S. Schultz-Fellenz, Colin J. Bray, Richard E. Kelley
A fine-grained, up to 3-m-thick tephra bed in southwestern Saskatchewan, herein named Duncairn tephra (Dt), is derived from an early Pleistocene eruption in the Jemez Mountains volcanic field of New Mexico, requiring a trajectory of northward tephra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::504d203c935203aa60beb0bac1208f08
http://hdl.handle.net/11585/801439
http://hdl.handle.net/11585/801439
Publikováno v:
Precambrian Research. 257:137-166
A paleomagnetic study of the western end of the ∼585 Ma Grenville dyke swarm shows that individual dykes are characterized by high coercivity and unblocking temperature magnetizations that can differ in direction by as much as 90°. Field tests inc
Publikováno v:
Precambrian Research. 244:1-4
Autor:
Henry C. Halls
Publikováno v:
Precambrian Research. 244:42-52
In the last 130 million years, perhaps as much as 2000 km of intra-continental shortening has taken place within Asia during 10,000 km of convergence between Siberia and India (with ∼8000 km being accommodated by oceanic subduction). Given that Ear
Autor:
Johanna Salminen, Henry C. Halls, Ulf Söderlund, Satu Mertanen, Lauri J. Pesonen, J.I. Vuollo
Publikováno v:
Precambrian Research. 244:87-99
Paleomagnetic results are presented for two Paleoproterozoic mafic dykes in the Taivalkoski area in northern Karelia Province of the Fennoscandian shield where, based on K-Ar data, the crust has seen minimal effects of the otherwise pervasive 1.8-1.9
Autor:
R. Don Russell, Henry C. Halls, Lawrence W. Morley, R. M. Farquhar, Gordon F. West, G.D. Garland
Publikováno v:
Canadian Journal of Earth Sciences. 51:xvii-xxxi
Fifty years ago, the world’s Earth Scientists experienced the so-called “Revolution in the Earth Sciences”. In the decade from 1960 to 1970, a massive convergence took place from many diverse and contradictory theories about the tectonic proces
Autor:
Henry C. Halls, Steven W. Denyszyn
Publikováno v:
Journal of Geophysical Research: Solid Earth. 119:360-363
Autor:
Henry C. Halls, David Evans
Publikováno v:
Precambrian Research. 183:474-489
Geometrical patterns of Paleoproterozoic dyke swarms in the Superior craton, North America, and paleomagnetic studies of those dykes, both indicate relative motion across the Kapuskasing Structural Zone (KSZ) that divides the craton into eastern and