Zobrazeno 1 - 4
of 4
pro vyhledávání: '"John M. U. Jocson"'
We report preliminary results of a field study of the natural discharge styles of a Pleistocene karst aquifer in uplifted Cenozoic coral-algal reef and lagoonal limestone. Discharge in deeply enscalloped embayments appears to be characterized by clos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3276f1e3792f739525e740606fe09573
https://doi.org/10.1201/9781003078128-2
https://doi.org/10.1201/9781003078128-2
Autor:
John M. U. Jocson, Blaž Miklavič, John E. Mylroie, Ethan Goddard, Judson W. Partin, Terrence M. Quinn, Frederick W. Taylor, John W. Jenson, Daniel J. Sinclair, Jay L. Banner
Publikováno v:
Chemical Geology. :1-17
We present bulk average Sr and Mg data for 13 speleothems from different locations in the western equatorial Pacific (Guam, Solomon Islands, and Vanuatu). These data plot on a single straight line in a graph of ln(Sr/Ca) vs ln(Mg/Ca) with a slope of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5871feb872a236689bfc98ca5f42328d
https://doi.org/10.1016/j.chemgeo.2011.10.008
https://doi.org/10.1016/j.chemgeo.2011.10.008
Publikováno v:
Journal of Hydrology. 260:231-254
The Northern Guam Lens Aquifer is an island karst aquifer in uplifted young, highly conductive limestone. Calculations of recharge based on differences between daily rainfall and daily pan evaporation suggest that the maximum annual mass of water del
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::915d53b3b05fa329dd78c4075754d2d1
https://doi.org/10.1016/s0022-1694(01)00617-5
https://doi.org/10.1016/s0022-1694(01)00617-5
Autor:
John W. Jenson, B. F. Hardt, Jay L. Banner, Danko Taboroši, John M. U. Jocson, Frederick W. Taylor, Blaž Miklavič, Mark A. Lander, D. J. Sinclair, Tomoko Bell, Judson W. Partin, Terrence M. Quinn
Publikováno v:
Geochemistry, Geophysics, Geosystems. 13
[1] Modern rainwater, cave dripwater and cave stalagmite geochemical time series from a cave in Guam (13°38′N, 144°53′E) are used to better understand how changes in cave stalagmite geochemistry relate to aboveground changes in rainfall at a tr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a8b7ce2771c25f6bbeade62053f8c3e8
https://doi.org/10.1029/2011gc003930
https://doi.org/10.1029/2011gc003930