Zobrazeno 1 - 10
of 39
pro vyhledávání: '"Nat Rutter"'
Publikováno v:
Journal of Asian Earth Sciences. 46:195-208
The objective of this research is to obtain a better understanding of the evolution of the Tunka rift basin, part of the Baikal rift zone, and how it relates to the overall geologic history of the region, particular for the Quaternary period. The tec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08f6d1b47c1cbd5300b7bd646a0d1788
https://doi.org/10.1016/j.jseaes.2011.12.010
https://doi.org/10.1016/j.jseaes.2011.12.010
Publikováno v:
Quaternary Science Reviews. 18:1351-1364
A 76.7 m-thick section of aeolian sediment is exposed in the transition zone between the Mu Us Desert and the Loess Plateau of northern China. The aeolian sediments contain sand beds, loess layers, and palaeosols. The particle-size distribution data
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63d75790dd61dddd95f22a54d027410d
https://doi.org/10.1016/s0277-3791(98)00086-9
https://doi.org/10.1016/s0277-3791(98)00086-9
Publikováno v:
Quaternary Science Reviews. 18:1205-1212
A high-resolution East Asian winter monsoon proxy record reconstructed from the Baoji loess section in China shows two major shifts in climate modes over the past 2.5 Ma, one occurring at about 1.7–1.6 Ma BP and the other at about 0.8–0.5 Ma BP.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::745d295a69ccfe631f7bd8f4c808bafe
https://doi.org/10.1016/s0277-3791(98)00110-3
https://doi.org/10.1016/s0277-3791(98)00110-3
Publikováno v:
Quaternary Research. 52:56-62
Geological records have shown that the deserts east of the Helan Mountains in northern China were covered by grass during the Holocene Optimum, whereas during marine oxygen isotope stages 2 and 4 distribution of the deserts was almost the same as at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bcadd37d73d6a54855df4f5900fbe677
https://doi.org/10.1006/qres.1999.2045
https://doi.org/10.1006/qres.1999.2045
Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine
Publikováno v:
Quaternary International. 40:53-60
In northern China the Red Clay-loess contact is palaeomagnetically defined at about the Gauss/Matuyama boundary. The Red Clay formation has recently been proposed as mostly of wind-blown origin, and can be interpreted as having been formed under clim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e6c97f51812d0898bfe0f486e07e2279
https://doi.org/10.1016/s1040-6182(96)00061-4
https://doi.org/10.1016/s1040-6182(96)00061-4
Publikováno v:
Quaternary Research. 44:149-159
Particle-size measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain size ratio of 10 μm (%) can be used as an indicator of variations in intensity of the East Asian wint
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4950eb8536c17a1e3e5660550d1822aa
https://doi.org/10.1006/qres.1995.1059
https://doi.org/10.1006/qres.1995.1059
Autor:
Nat Rutter
Publikováno v:
Quaternary International. 28:19-37
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::721741479ff723c169669fad9dbfad54
https://doi.org/10.1016/1040-6182(95)00045-k
https://doi.org/10.1016/1040-6182(95)00045-k
Publikováno v:
SpringerBriefs in Earth System Sciences ISBN: 9789400743984
The geomorphological, sedimentary and pedological evidence related to the various glacial periods which took place in the Patagonian and Fuegian Andes between the Late Miocene and the Late Pleistocene are herein presented and discussed. The occurrenc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a9dfd315c2ca072d8ef1f5b0888ead5f
https://doi.org/10.1007/978-94-007-4399-1_1
https://doi.org/10.1007/978-94-007-4399-1_1
Publikováno v:
SpringerBriefs in Earth System Sciences ISBN: 9789400743984
The Bogota basin and direct surroundings (eastern Andes in Colombia) holds a long sedimentary sequence that reaches from the present into the Miocene. Palaeo-botanical data indicates tectonic uplift by some 2,000 m during the Late Miocene–Pliocene
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a3f2db2c559346b0b1b091ca13efe46
https://doi.org/10.1007/978-94-007-4399-1_2
https://doi.org/10.1007/978-94-007-4399-1_2