Zobrazeno 1 - 8
of 8
pro vyhledávání: '"M. S. Money"'
Publikováno v:
Quarterly Journal of Engineering Geology. 31:211-234
The landscape of Northern England has been subjected to glacial activity several times during the Quaternary period. Successive ice sheets may have ‘swept clear’ the bedrock surface in places, but may also have incorporated materials from previou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91d3fb4b63954fbeeef68885740af79c
https://doi.org/10.1144/gsl.qjeg.1998.031.p3.05
https://doi.org/10.1144/gsl.qjeg.1998.031.p3.05
Publikováno v:
Proceedings of the Institution of Civil Engineers - Municipal Engineer. 109:212-232
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe8aebbc87eadbb4051c428b562b5945
https://doi.org/10.1680/imuen.1995.28024
https://doi.org/10.1680/imuen.1995.28024
Publikováno v:
Bulletin of the International Association of Engineering Geology. 29:355-359
The Whin Sill is a dolerite intrusion with extensive outcrops in North East England. Quarries in the sill, provide the bulk of the crushed rock aggregates in the region suitable for roadstone. The dolerite is generally of high strength and little aff
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a66981f0083ef6c88ccaebd654a92218
https://doi.org/10.1007/bf02594435
https://doi.org/10.1007/bf02594435
Publikováno v:
Bulletin of the International Association of Engineering Geology. 19:5-17
The initial results of an engineering geological survey of the Tyne and Wear Conurbation in North-east England are presented in the form of maps prepared at a scale of 1∶50,000 and reproduced at a scale of 1∶200,000. Separate maps are presented o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::190bb507d581738cb22f4f0d386c9b81
https://doi.org/10.1007/bf02600441
https://doi.org/10.1007/bf02600441
Publikováno v:
Bulletin of the International Association of Engineering Geology. 18:179-185
Magnetic and resistivity surveys have been carried out over abandoned mine-shafts in a rural area free from background noise. The results are compared with those from a similar survey in an urban area and with anomalies predicted from computer and sm
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a1bf039378c26d71c225793a19b9342
https://doi.org/10.1007/bf02635368
https://doi.org/10.1007/bf02635368
Publikováno v:
Quarterly Journal of Engineering Geology. 10:145-168
Summary Preparation of an engineering geological map of the Tyne and Wear Metropolitan County, North-East England from available archival, geological and site investigation data has involved appraisal of the general engineering geological conditions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::60cad0151173583c80f13502fe2550f0
https://doi.org/10.1144/gsl.qjeg.1977.010.02.04
https://doi.org/10.1144/gsl.qjeg.1977.010.02.04
Autor:
M. S. Money, I. M. Platten
Publikováno v:
Transactions of the Royal Society of Edinburgh: Earth Sciences. 78:85-103
Pipe-shaped breccia bodies associated with diorite intrusions are composed mainly of angular clasts of local schists with a few transported clasts of quartzite. Plate shaped fragments are commonly oriented to define planar fabrics in the breccias. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::490aa00a872fea9af75e3a901fb82c93
https://doi.org/10.1017/s0263593300011007
https://doi.org/10.1017/s0263593300011007
Autor:
M. S. Money, R. Pearson
Publikováno v:
Quarterly Journal of Engineering Geology. 10:221-239
Summary The Lugeon or packer test for estimating rock permeability is not standardized and often yields anomalous results. A programme of repeated tests has been carried out in shallow drillholes in sandstones and greywackes making use of constant he
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3eda9abc6c0ac5846e3f316c033b74ab
https://doi.org/10.1144/gsl.qjeg.1977.010.03.05
https://doi.org/10.1144/gsl.qjeg.1977.010.03.05