• 検索結果がありません。

Late Pleistocence and Holocence environmental changes recorded in the terrestrial sediments and landforms of Eastern Siberia and North Mongolia

N/A
N/A
Protected

Academic year: 2022

シェア "Late Pleistocence and Holocence environmental changes recorded in the terrestrial sediments and landforms of Eastern Siberia and North Mongolia"

Copied!
8
0
0

読み込み中.... (全文を見る)

全文

(1)

Late Pleistocence and Holocence environmental changes recorded in the terrestrial sediments and landforms of Eastern Siberia and North Mongolia

著者 Krivonogov Sergey K., Takahara Hikaru journal or

publication title

Proceedings, International Symposium of the Kanazawa University 21st‑Century COE Program

volume 1

page range 30‑36

year 2003‑03‑16

URL http://hdl.handle.net/2297/6359

(2)
(3)
(4)
(5)
(6)
(7)
(8)

参照

関連したドキュメント

熱力学計算によれば、この地下水中において安定なのは FeSe 2 (cr)で、Se 濃度はこの固相の 溶解度である 10 -9 ~10 -8 mol dm

Osawa Takashi, 2017, The position and significance of the inscription and site of Dongoin Shiree of the Eastern Mongolia in the Archaeological and Historical research

The mGoI framework provides token machine semantics of effectful computations, namely computations with algebraic effects, in which effectful λ-terms are translated to transducers..

Standard domino tableaux have already been considered by many authors [33], [6], [34], [8], [1], but, to the best of our knowledge, the expression of the

We shall give a method for systematic computation of γ K , give some general upper and lower bounds, and study three special cases more closely, including that of curves with

H ernández , Positive and free boundary solutions to singular nonlinear elliptic problems with absorption; An overview and open problems, in: Proceedings of the Variational

Keywords: Convex order ; Fréchet distribution ; Median ; Mittag-Leffler distribution ; Mittag- Leffler function ; Stable distribution ; Stochastic order.. AMS MSC 2010: Primary 60E05

The set of families K that we shall consider includes the family of real or imaginary quadratic fields, that of real biquadratic fields, the full cyclotomic fields, their maximal