Zobrazeno 1 - 10
of 93
pro vyhledávání: '"Mark M. Fenton"'
Autor:
Anthony N. Sartorelli, Michael S. Pesowski, James D. Henderson, Mark M. Fenton, Donald H. Green
Publikováno v:
Geotechnical Stability in Surface Mining ISBN: 9781003079286
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5fd8302ff80c36bfd426685eef34cc9
https://doi.org/10.1201/9781003079286-35
https://doi.org/10.1201/9781003079286-35
Autor:
Mark M. Fenton, Mark R. Trudell, John G. Pawlowicz, Carolyn E. Jones, Stephen R. Moran, D.J. Nikols
Publikováno v:
Geotechnical Stability in Surface Mining ISBN: 9781003079286
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c143cad556c02c7837050e8d37a6cf0c
https://doi.org/10.1201/9781003079286-34
https://doi.org/10.1201/9781003079286-34
Autor:
Mark M. Fenton, Mark R. Trudell, John G. Pawlowicz, Carolyn E. Sterenberg, Stephen R. Moran, Dennis J. Nikols
Publikováno v:
Applied Quaternary Research ISBN: 9781003079309
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::85e7a7749352336f362581b34f49b206
https://doi.org/10.1201/9781003079309-2
https://doi.org/10.1201/9781003079309-2
Autor:
James T. Teller, Mark M. Fenton
Publikováno v:
Canadian Journal of Earth Sciences. 17:19-35
The history of Late Wisconsinan glaciation in southwestern Manitoba has been established by identifying and correlating ice-laid lithostratigraphic units in the subsurface. Five Late Wisconsinan tills are defined on the basis of their texture, minera
Autor:
Leo S. Luckinbill, Mark M. Fenton
Publikováno v:
Ecology. 59:1271-1276
Regulation of population size is described for 2 protozoan species in environments that become progressively more variable in time. The ciliate, Colpidium campylum, rapidly adjusts pop- ulation levels to fixed equilibria set by bacterial food supply.
Publikováno v:
Glaciotectonic Landforms and Structures ISBN: 9789401568432
Glaciotectonic features were considered unusual or rare glacial phenomena when first recognized more than a century ago. This point of view persisted for a long time, because the documented examples of glaciotectonic landforms and structures were few
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a0a5a7d689a21c86ed8280100ef2ef14
https://doi.org/10.1007/978-94-015-6841-8_9
https://doi.org/10.1007/978-94-015-6841-8_9
Publikováno v:
Glaciotectonic Landforms and Structures ISBN: 9789401568432
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba88953eb8ba8acf6437d1d414dcd0ee
https://doi.org/10.1007/978-94-015-6841-8_8
https://doi.org/10.1007/978-94-015-6841-8_8
Publikováno v:
Glaciotectonic Landforms and Structures ISBN: 9789401568432
The most typical and distinctive glaciotectonic landforms are ice-shoved ridges found in many glaciated plains. Prest (1983:45) aptly described such ridges as, ‘a composite of great slices of up-thrust and commonly contorted sedimentary bedrock tha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66584c7953a5e60c4bc05884bf590e1c
https://doi.org/10.1007/978-94-015-6841-8_3
https://doi.org/10.1007/978-94-015-6841-8_3