Zobrazeno 1 - 6
of 6
pro vyhledávání: '"David Krinsley"'
Autor:
Sam Boggs, David Krinsley
Minerals in sedimentary rocks emit characteristic visible luminescence called cathodoluminescence (CL) when bombarded by high energy electrons. CL emissions can be displayed as colour images in a cathodoluminescence microscope or as high-resolution m
Publikováno v:
Astrobiology; Aug2009, Vol. 9 Issue 6, p551-562, 12p
Autor:
David Krinsley, Thomas R. Mckee
Publikováno v:
Proceedings, annual meeting, Electron Microscopy Society of America. 36:486-487
Although sand and silt-sized quartz have been studied extensively, clay-sized quartz has received scant attention, despite the fact that its nature and production are of considerable interest to sedimentologists, geochemists, and workers in the field
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71f5a8fb4cb1fb2fdaf61961ac22b529
https://doi.org/10.1017/s0424820100109574
https://doi.org/10.1017/s0424820100109574
Autor:
DAVID KRINSLEY
Publikováno v:
Sedimentology. 28:740-740
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::60e32c9157e3a5db8fd1aa7be0a43635
https://doi.org/10.1111/j.1365-3091.1981.tb01937.x
https://doi.org/10.1111/j.1365-3091.1981.tb01937.x
Autor:
David Krinsley, Peter Hyde
Publikováno v:
Micropaleontology. 10:491
A simplified technique for preparing replicas of broken surfaces, complete surfaces or broken sections of foraminifera for examination by electron microscopy is presented. The technique produces ultrathin films which are usable 90 percent of the time
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0e4d75e40be149b25cea3a29258cf039
https://doi.org/10.2307/1484659
https://doi.org/10.2307/1484659
Autor:
David Krinsley
Publikováno v:
Micropaleontology. 6:297
Seven trace elements - Mn, Ti, Al, Mg, Sr, Cu, and Ni - were examined in the tests of planktonic foraminifera in cores from the Atlantic Ocean. Mn concentrations appear to be related to geographic location; Cu is probably stable in planktonic foramin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::542bc65f537e8ba383b76bb508922fdc
https://doi.org/10.2307/1484237
https://doi.org/10.2307/1484237