GEOLOGICAL STUDY OF THE DEPOSITS OF THE SANGKANHO BASIN.

GEOLOGICAL STUDY OF THE DEPOSITS OF THE SANGKANHO BASIN.
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DOI:
10.1111/j.1755-6724.1926.mp53-4005.x
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发表时间:
2009-05
期刊:
Bulletin of The Geological Society of China
影响因子:
--
通讯作者:
G. Barbour;E. Licent;P. Chardin
G. Barbour;E. Licent;P. Chardin
中科院分区:
其他
文献类型:
--
作者:
G. Barbour;E. Licent;P. Chardin

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他们一进入西安平原就遇到了。nlng。chitli, hsien(见第五章)。1) 000人占据了上溪河和侯河交界处的整个大盆地。林。何*。在Sangkanho地区的山谷中,他们遇到了片麻岩和古生代沉积物的屏障,这些沉积物横亘在河流的峡谷中。西北方向。而对西方来说,由于后来的侵蚀,它们可能会逐渐消失。ning-hiien平原。
They are met on entering the plain of Hsi. nlng. hsien, Chtbli (see Ffg. l) 000upying the whole of the large basin at the junction of the Sangksnho and the HOU. lin. ho*. In the valley of the Sangkanho proper, they abut ag&mst the barrier of gneiss and paleozoic sediments that lie athwart the gorge of the river in a BE. NW direction. While to the West: they thin outposibly owing to later eroslouand disappear under the Hsi. ning-hiien plain.