Zobrazeno 1 - 10
of 76
pro vyhledávání: '"Rodney Grapes"'
Publikováno v:
CATENA. 167:305-318
A layer of yellow silt with thickness from tens of centimeters to a few meters is widely distributed on low hills and terraces in the coastal area of south China. The yellow silt has different sedimentological characteristics from other common types
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::17659cc10143418c4d08063bc679f804
https://doi.org/10.1016/j.catena.2018.04.032
https://doi.org/10.1016/j.catena.2018.04.032
Publikováno v:
Aeolian Research. 19:113-122
A layer of yellow silt is widely distributed in the late Quaternary succession of the Pearl River delta, southeast China. A representative section at Xi Lingang was analyzed using particle size analysis, scanning electron microscope observation, geoc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa989b6337caec0b8216a9038cd8e967
https://doi.org/10.1016/j.aeolia.2015.09.005
https://doi.org/10.1016/j.aeolia.2015.09.005
Publikováno v:
Journal of Asian Earth Sciences. 101:14-19
The origin of continental red beds in SE China is the result of high diagenetic temperatures, rather than an arid climate during their deposition. Here we present results from an experimental study where black mud was heated to demonstrate the format
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb5db96391fc53a83f812f26654c5da6
https://doi.org/10.1016/j.jseaes.2015.01.019
https://doi.org/10.1016/j.jseaes.2015.01.019
Autor:
Guy R. Holdgate, Rodney Grapes
Publikováno v:
Australian Journal of Earth Sciences. 62:95-121
Cook Strait separates North Island and South Island of New Zealand. It contains the Wairau and other sedimentary basins, which have sedimentary thicknesses of up to 4 km. The Strait overlies part of the Australia–Pacific plate boundary where subduc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02effad7af946259d5701b059f9e14f4
https://doi.org/10.1080/08120099.2015.986195
https://doi.org/10.1080/08120099.2015.986195
Autor:
Rodney Grapes, Guy R. Holdgate
Publikováno v:
New Zealand Journal of Geology and Geophysics. 57:312-330
The 1848 and 1855 earthquakes provide examples of clustered earthquake sequences involving several faults. Historical evidence indicates that fault rupturing and ground deformation on both sides of Cook Strait occurred over periods of several days du
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f6b261405391d43dd362d1a2a73b72d
https://doi.org/10.1080/00288306.2014.907579
https://doi.org/10.1080/00288306.2014.907579
Publikováno v:
Contributions to Mineralogy and Petrology. 165:781-803
High-Na slag-like rocks (paralava) with 4.5–11 % Na2O from the Altyn-Emel mud volcanic field, Kazakhstan, are the products of melting of sediment + salt mixtures by methane flares associated with mud extrusion. The main minerals of the paralavas ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8529ee2190d3466e2b4a3791410c99de
https://doi.org/10.1007/s00410-012-0835-4
https://doi.org/10.1007/s00410-012-0835-4
Publikováno v:
Journal of Asian Earth Sciences. 56:33-41
A Late Cretaceous tempestite in the northern Songliao Basin, China, was studied based on thin-section and granularity analyses of borehole samples. The results indicated that the local tempestite can be categorized into several clastic constituent ty
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0928cc0894757ae7206986454a0f3b88
https://doi.org/10.1016/j.jseaes.2012.02.007
https://doi.org/10.1016/j.jseaes.2012.02.007
Publikováno v:
Lithos. 120:347-367
The origin of high-Mg adakitic granitoids in collisional orogens can provide important information about the nature of the lower crust and upper mantle during the orogenic process. Late-Triassic high-Mg adakitic granite and its mafic enclaves from th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c64c3218ebbbc24ac859caaf5cb0cf52
https://doi.org/10.1016/j.lithos.2010.08.022
https://doi.org/10.1016/j.lithos.2010.08.022
Publikováno v:
Contributions to Mineralogy and Petrology. 162:253-273
Sekaninaite (XFe > 0.5)-bearing paralava and clinker are the products of ancient combustion metamorphism in the western part of the Kuznetsk coal basin, Siberia. The combustion metamorphic rocks typically occur as clinker beds and breccias consisting
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01c8d6b076fada4144fe373712d4911b
https://doi.org/10.1007/s00410-010-0593-0
https://doi.org/10.1007/s00410-010-0593-0
Autor:
Jörg Keller, Rodney Grapes
Publikováno v:
European Journal of Mineralogy. 22:285-292
Fe-dominant rhonite with between 25 and 28 wt% FeO (as total iron) occurs as a late crystallizing phase in tephrite and limburgite from the Kaiserstuhl volcanic complex, Upper Rhine Graben, Germany. Average compositions are: (K 0.05 Na 0.40 Ca 1.55 )
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b9082691740de5a0587d0866c0435ae9
https://doi.org/10.1127/0935-1221/2010/0022-1996
https://doi.org/10.1127/0935-1221/2010/0022-1996