Zobrazeno 1 - 10
of 58
pro vyhledávání: '"M. R. Leeder"'
Autor:
M. R. Leeder
Publikováno v:
Geological Journal. 11:21-28
The alluvial depositional surface of the Scottish Border Basin in youngest Upper Old Red Sandstone times is thought to have been dissected and subsequently disrupted and buried as an effect of magma formation and lava eruption. Lengthy periods of sur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6dcc98df41f85f1d8328fc0a25e50398
https://doi.org/10.1002/gj.3350110103
https://doi.org/10.1002/gj.3350110103
Autor:
R. L. Gawthorpe, M. R. Leeder
Publikováno v:
Basin Research. 12:195-218
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71a97dd2fe26bd12c94d7c60e8d7e1da
https://doi.org/10.1046/j.1365-2117.2000.00121.x
https://doi.org/10.1046/j.1365-2117.2000.00121.x
Autor:
M. R. Leeder, M. D. Stewart
Publikováno v:
Geological Society, London, Special Publications. 103:25-39
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15a630769373abcda5bfc8ac61d55036
https://doi.org/10.1144/gsl.sp.1996.103.01.03
https://doi.org/10.1144/gsl.sp.1996.103.01.03
Autor:
M. R. Leeder
Publikováno v:
Geological Society, London, Special Publications. 73:7-22
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c0fdea98a569159cdf18f2b55241767a
https://doi.org/10.1144/gsl.sp.1993.073.01.02
https://doi.org/10.1144/gsl.sp.1993.073.01.02
Autor:
M. R. Leeder
Publikováno v:
Modern and Ancient Fluvial Systems
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d2ed1dcbb54ee2455daff2ed6e74fefd
https://doi.org/10.1002/9781444303773.ch1
https://doi.org/10.1002/9781444303773.ch1
Publikováno v:
Journal of the Geological Society. 148:331-343
The active Psatha–Skinos normal fault is uplifting a contrasting variety of lithologies in its footwall, including Mesozoic limestones, ophiolitic peridotites and poorly-consolidated Plio-Pleistocene sediments of the inactive Megara basin. In the l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b8db7ccfc524dda54fa6c29fb2ce5fe9
https://doi.org/10.1144/gsjgs.148.2.0331
https://doi.org/10.1144/gsjgs.148.2.0331
Autor:
M. R. Leeder
Publikováno v:
Proceedings of the Yorkshire Geological Society. 40:129-180
Summary Lower Border Group (Tournaisian) successions in the Northumberland basin are divided into seven formations. Only broad correlation between laterally equivalent formations is possible owing to facies changes. Facies association 1 comprises thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::abef6ed4a984eb873d4d69589885f77c
https://doi.org/10.1144/pygs.40.2.129
https://doi.org/10.1144/pygs.40.2.129
Autor:
M. R. Leeder
Publikováno v:
Scottish Journal of Geology. 10:283-296
Synopsis The Northumberland basin was initiated after eruption of alkali basalts onto the alluvial plains of the Upper Old Red Sandstone Scottish Border basin. The Birrenswark and Kelso Lavas are postulated as of upper mantle origin, produced by part
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a3e27e4cef0ded9e380133ced8ac2ca3
https://doi.org/10.1144/sjg10040283
https://doi.org/10.1144/sjg10040283
Autor:
M. R. Leeder, M. Nami
Publikováno v:
Proceedings of the Yorkshire Geological Society. 42:461-482
SUMMARY Alternative alluvial and deltaic depositional models for the topmost Scarborough and Scalby Formation are outlined. Biostratigraphical and sedimentological arguments are used to deduce that a lengthy time gap of around 9.0 m.y. existed betwee
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d479be206b7dd840b95c71e6ad26f49c
https://doi.org/10.1144/pygs.42.3.461
https://doi.org/10.1144/pygs.42.3.461