Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Joseph D. Martinez"'
Autor:
Robert Boehner, Joseph D. Martinez
Publikováno v:
Carbonates and Evaporites. 12:84-90
Nova Scotia contains enormous deposits of Windsor Group (Mississippian) gypsum overlain by extensive late Wisconsian glacial drift. A variety of dissolution karst structures and land forms are the outstanding feature of many areas underlain by gypsum
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::46eec02a2b49df1858d7dd8d218f1f22
https://doi.org/10.1007/bf03175806
https://doi.org/10.1007/bf03175806
Publikováno v:
American Scientist. 86:38
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c46aea89e35f97e73e7e604b3d55aaa
https://doi.org/10.1511/1998.1.38
https://doi.org/10.1511/1998.1.38
Autor:
Joseph D. Martinez
Publikováno v:
Eos, Transactions American Geophysical Union. 72:259-259
Forensic geology binds applied geology to the world of legal controversy and action. However, the term “forensic” is often misconstrued. Although even some attorneys apply it only to the marshalling of evidence in criminal cases, it has a much br
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a0c341f894d6a144ab4f4234aa1281d4
https://doi.org/10.1029/90eo10199
https://doi.org/10.1029/90eo10199
Publikováno v:
Journal of Hydrology. 54:107-140
Kumar, M.B. and Martinez, J.D., 1981. Character of brines from the Belle Isle and Weeks Island salt mines, Louisiana, U.S.A. In: W. Back and R. Letolle (Guest-Editors), Symposium on Geochemistry of Groundwater — 26th International Geological Congre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b93163f80f73275731928be6aeb8f31
https://doi.org/10.1016/0022-1694(81)90155-4
https://doi.org/10.1016/0022-1694(81)90155-4
Autor:
Joseph D. Martinez
Publikováno v:
Environmental & Engineering Geoscience. :93-100
Contrasting views of a potential Mississippi River diversion were presented in 1980. Kazmann and Johnson (1980) predicted dire results from a future failure of the Old River Control Structure which was constructed to prevent diversion of the Mississi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a00b68f537011d396d0b8fac3aec0d2
https://doi.org/10.2113/gseegeosci.xxiii.1.93
https://doi.org/10.2113/gseegeosci.xxiii.1.93
Publikováno v:
GEOPHYSICS. 25:1094-1099
Previously obtained magnetic data for Silurian samples from Alabama are presented. Both the remanent vector and the plane of maximum susceptibility lie close to the bedding plane for this ore containing chemically formed hematite. Now, X‐ray measur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4d5d872b67721f3c76b8f48c565a7c16
https://doi.org/10.1190/1.1438791
https://doi.org/10.1190/1.1438791
Publikováno v:
Environmental Letters. 4:311-316
Measurements using atomic absorption spectrometry have established the prescence of Pb, Hg, Cd, Zn, Cu, and Cr in shells of the oyster Crassostrea virginica in amounts considerably higher than their concentration in sea water. Preliminary comparisons
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::31c502b47ca77648183a67bbe1c7b3cf
https://doi.org/10.1080/00139307309435502
https://doi.org/10.1080/00139307309435502
Publikováno v:
GEOPHYSICS. 23:285-298
It seems that in general the plane of maximum magnetic susceptibility lies in the bedding plane for sediments and in the plane of foliation for metamorphic rocks; there is, also, a tendency for the remanent vector to lie in the plane of foliation in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4b3ba2d6f400c8c0689c3b1a73c4f87
https://doi.org/10.1190/1.1438469
https://doi.org/10.1190/1.1438469
Autor:
Lynn Gorman Howell, Joseph D. Martinez
Publikováno v:
GEOPHYSICS. 22:384-397
Measurements of remanent magnetism have been carried out by geophysicists both in this country and in the British Isles in a broad sampling of Paleozoic sediments. The direction of magnetization of these rocks indicates that the positions of the eart
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a63eb81d302969e938060bdde716117
https://doi.org/10.1190/1.1438371
https://doi.org/10.1190/1.1438371