Research in China volume 2
Research in China volume 2
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In our eReader you can find the full English version of the book. Read Research in China volume 2 Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Research in China volume 2
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F Ibid. , bottom of page 235. %Ibid. , page 236. THE WESTERN KUEN-LUNG. 63 the series of gray schists, quartzites, and limestones, is considered older than that of gray, green, and lilac shales, which we take for Devonian. " These older schists, quartzites, and limestones belong to that series which has been considered early Paleozoic, but which I correlate tentatively with the late Proterozoic. I shall refer to it again in connection with Pale- ozoic diastrophism. Having referred briefly to th...e structure of the fourth chain, which is but imperfectly known, but which is undoubtedly formed by beds of Paleozoic strata, in part at least, Suess proceeds:* The structure of these four ranges of the Nan-shan, from the oasis of Kan-su to the vicinity of the valley of Bouk-hai'n-gol thus presents the following characteristics: gneiss is seen only upon the southern flank of the To-lai'-shan; all the rest of the mountainous region is formed of closely folded Paleozoic sediments. Near the northern margin there are suggestions of an overturn toward the north ; in the interior of the mountains the beds appear in a vertical position or exhibit a movement toward the south.
What to read after Research in China volume 2?
You can find similar books in the "Read Also" column, or choose other free books by Carnegie Institution of Washington to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
F Ibid. , bottom of page 235. %Ibid. , page 236. THE WESTERN KUEN-LUNG. 63 the series of gray schists, quartzites, and limestones, is considered older than that of gray, green, and lilac shales, which we take for Devonian. " These older schists, quartzites, and limestones belong to that series which has been considered early Paleozoic, but which I correlate tentatively with the late Proterozoic. I shall refer to it again in connection with Pale- ozoic diastrophism. Having referred briefly to th...e structure of the fourth chain, which is but imperfectly known, but which is undoubtedly formed by beds of Paleozoic strata, in part at least, Suess proceeds:* The structure of these four ranges of the Nan-shan, from the oasis of Kan-su to the vicinity of the valley of Bouk-hai'n-gol thus presents the following characteristics: gneiss is seen only upon the southern flank of the To-lai'-shan; all the rest of the mountainous region is formed of closely folded Paleozoic sediments. Near the northern margin there are suggestions of an overturn toward the north ; in the interior of the mountains the beds appear in a vertical position or exhibit a movement toward the south.
What to read after Research in China volume 2?
You can find similar books in the "Read Also" column, or choose other free books by Carnegie Institution of Washington to read onlineMoreLess
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