Zobrazeno 1 - 10
of 25
pro vyhledávání: '"F. Leo Lynch"'
Publikováno v:
Journal of Sedimentary Research. 74:858-867
When biofilms (aggregations of bacteria and extracellular polymer secretions) in samples from the Carter Sandstone of Alabama were prepared for scanning electron microscopy (SEM) using different dehydration techniques, the organic material had visibl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2f7d5574395fffa4fe14f5e6164b048
https://doi.org/10.1306/042604740858
https://doi.org/10.1306/042604740858
Autor:
Robert L. Folk, F. Leo Lynch
Publikováno v:
Sedimentology. 48:215-229
Modern ooids from Joulters Cay, when baked at 500 °C, turn various shades of black depending upon the organic content. Mucus-rich laminae occur at quasi-regular intervals of a few micrometres within the cortex. When mucus is still present, it turns
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::68ae5d2e23dbf29ff3a1c42a17a1b7cc
https://doi.org/10.1046/j.1365-3091.2001.00354.x
https://doi.org/10.1046/j.1365-3091.2001.00354.x
Publikováno v:
Sedimentary Geology. 126:243-252
Scanning electron microscopy reveals an association between early dolomite in the Pennsylvanian Desert Creek (Paradox Fm.) and small (approximately 0.1 μm) nanometer-scale textures, termed `nannobacteria'. Three diagenetically distinct dolomites are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b600560d914b464025f55b54d5e681cc
https://doi.org/10.1016/s0037-0738(99)00043-3
https://doi.org/10.1016/s0037-0738(99)00043-3
Autor:
F. Leo Lynch, Barbara J. Mahler
Publikováno v:
Journal of Hydrology. 214:165-178
Karst aquifers are capable of transporting and discharging large quantities of suspended sediment, which can have an important impact on water quality. Here we present the results of intensive monitoring of sediment discharging from a karst spring in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a9ea1a4b0555666a9897748f230085d
https://doi.org/10.1016/s0022-1694(98)00287-x
https://doi.org/10.1016/s0022-1694(98)00287-x
Publikováno v:
Geochimica et Cosmochimica Acta. 61:1995-2006
Several gram-size samples of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c37343f7b465a2e8a9f717d6fed47f35
https://doi.org/10.1016/s0016-7037(97)00066-5
https://doi.org/10.1016/s0016-7037(97)00066-5
Publikováno v:
Geological Society of America Bulletin. 109:2-15
Cuttings from a well through a thick section of Miocene–Oligocene mudrocks from Kenedy County, Texas, spanning a depth range of 2130 to 5490 m (7000 to 18 000 ft), have been studied petrographically and geochemically. On the basis of whole-rock che
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::234d49afd3d48d04897837f97ffe1884
https://doi.org/10.1130/0016-7606(1997)109<0002:bdoass>2.3.co
https://doi.org/10.1130/0016-7606(1997)109<0002:bdoass>2.3.co
Autor:
F. Leo Lynch
Publikováno v:
Clays and Clay Minerals. 45:618-631
Burial diagenesis of shales of the Frio Formation resulted in an increase in the abundance of mixed-layer illite-smectite (I-S), albite and chlorite, and a decrease in the abundance of K-feldspar, illite and kaolinite. Some of the mineralogic trends
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10412eb10da76fa5f06a8668bb5b5f1e
https://doi.org/10.1346/ccmn.1997.0450502
https://doi.org/10.1346/ccmn.1997.0450502
Autor:
F. Leo Lynch, Lynton S. Land
Publikováno v:
Geochimica et Cosmochimica Acta. 60:3347-3352
The whole-rock δ 18 O of mudrocks, as well as the δ 18 O of the clay-sized silicate fraction, does not change in any systematic manner over Paleozoic and late Proterozoic time. Therefore, the δ 18 O of the ocean has not changed (except a per mil o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c4bc8a1944c7c8a07d53470d36fc156
https://doi.org/10.1016/0016-7037(96)00185-8
https://doi.org/10.1016/0016-7037(96)00185-8
Autor:
William K. Funderburk, F. Leo Lynch, Darrel Schmitz, Lewis R. Brown, Krystal M. Collins, Brenda L. Kirkland
The objective of this project was to couple microbial permeability profile modification (MPPM), with carbon dioxide flooding to improve oil recovery from the Upper Cretaceous Little Creek Oil Field situated in Lincoln and Pike counties, MS. This stud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad7fe740fba3fe6f95ab2521bbf3f7e4
https://doi.org/10.2172/1013260
https://doi.org/10.2172/1013260
Publikováno v:
Studies of Cave Sediments ISBN: 9781461347996
Studies of Cave Sediments ISBN: 9781402053269
Studies of Cave Sediments ISBN: 9781402053269
The unusual characteristics of subterranean flow in karst aquifers allow for the transport of sediment. Karst ground-water systems are created by dissolution of the bedrock matrix coupled with structural and stratigraphic controls. As a result, high
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d9b212e559f3778fdb59fe93430d00b7
https://doi.org/10.1007/978-1-4419-9118-8_2
https://doi.org/10.1007/978-1-4419-9118-8_2