国立情報学研究所 - ディジタル・シルクロード・プロジェクト
『東洋文庫所蔵』貴重書デジタルアーカイブ
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| 0262 |
Southern Tibet : vol.3 |
| 南チベット : vol.3 |
引用情報
OCR読み取り結果
How little the geology was known may be seen from the following passage,
dealing with STOLICZKA's section in the west: »It cannot be supposed that the rough
cross section we have sketched near the west end of the Tibetan mountain mass
can be taken as a type for the immense region to the east. Already within known
ground, some interruptions can be pointed out to the longitudinal extension of the
several structural zones. Of the continuation of the Karakorum and Kuen luen, and
even of the middle gneissic range, we may be said to know nothing. Stoliczka
describes the nummulitic band as completely stopped out against the syenite at Kargil;
and although this obtruding rock is at least in part of later date, it is suggested
that the termination of the eocene beds here is probably aboriginal. The eastern
extension of these deposits is quite unknown, save that nummulitic strata occur in
the far east north of Sikkim.»
Atkinson is right. It would be ridiculous to expect even the remotest know-
ledge of the geology further east from the scanty researches carried out in the west.
We have seen that the information brought back by Pundits from west and east is
not sufficient to interpolate the orography of the central parts of our system. How
much less then the geology! Only the eight geological profiles I have made across
the system, compared with the researches of the Stracheys, Godwin-Austen, Hay-
den and others, and which are elaborated and published by Professor A. HENNIG
as Vol. V of the present work, will give an idea of the geological structure of the
Transhimalaya.¹
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349
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563
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575
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587
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599
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610
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