Ascendancy
发表于 2025-3-25 05:39:39
http://reply.papertrans.cn/63/6240/623929/623929_21.png
Crater
发表于 2025-3-25 10:28:45
C. Tarquin Teale,Jeremy R. Young. The analysis of this media discourse is critical to understanding the support enjoyed by the armed forces in power: the vast majority of the population was not informed about the disappearances or the concent978-1-349-95774-3978-1-349-95251-9
原始
发表于 2025-3-25 14:05:12
http://reply.papertrans.cn/63/6240/623929/623929_23.png
精确
发表于 2025-3-25 15:54:04
see such precocious talent combined with such a caring, modest and well-balanced personality. He was des tined for the highest honours in geoscience and there is no doubt that he would have lived a life, had he been granted the chance, which would have spread colour, intellectual insight and goodness.978-94-010-7954-9978-94-009-3241-8
方舟
发表于 2025-3-25 21:52:28
Comparing Examples of Modern and Ancient Turbidite Systems: Problems and Concepts, selected for comparison must represent depositional systems similar in such characteristics as type of basin, size of sediment source, physical and temporal scales, and stage of development. Many fan sedimentation models presently in use do not meet these criteria..A conceptual framework for compar
GOAD
发表于 2025-3-26 04:04:02
An Example of the Use of Detrital Episodes in Elucidating Complex Basin Histories: the Caloveto andution of the basins in which the strata were deposited. The main episodes appear to be related to: (1) rifting and transgression over a crystalline basement and birth of a carbonate platform (Middle Lias); (2) progressive collapsing and drowning of the platform (Late Lias); (3) further extension of
凹槽
发表于 2025-3-26 04:48:31
http://reply.papertrans.cn/63/6240/623929/623929_27.png
清真寺
发表于 2025-3-26 09:59:07
http://reply.papertrans.cn/63/6240/623929/623929_28.png
ostracize
发表于 2025-3-26 15:33:36
http://reply.papertrans.cn/63/6240/623929/623929_29.png
entitle
发表于 2025-3-26 20:21:30
Evolution of Silurian Depositional Systems in the Southern Uplands, Scotland,nt dispersal parallel to the margin consistent with the presence of a topographic trench. Mid-Silurian sequences, however, record a major change in the character of sedimentation at the north-west margin of the Iapetus ocean. Early Wenlock depositional trends follow those of the Upper Llandovery. In