Full resolution (JPEG) - On this page / på denna sida - Sidor ...
<< prev. page << föreg. sida << >> nästa sida >> next page >>
Below is the raw OCR text
from the above scanned image.
Do you see an error? Proofread the page now!
Här nedan syns maskintolkade texten från faksimilbilden ovan.
Ser du något fel? Korrekturläs sidan nu!
This page has never been proofread. / Denna sida har aldrig korrekturlästs.
60
Udekomponeret
af
Saltsyre
44.43 pCt.
fjernoxyd.... 3.29
[Lerjord ... 8.81
Spor
I Magnesia .
[Kiselsyre (dek.iigidtk.’i . 32.33
Sum 99.90
Samlede Bestanddele:
FeO Fea03
0.92 7.24
A1,03
13.52
CaO
0.42
MgO
1.94
CaC03
41.18
r,,oä
Spor
Glodn.tab
2.35
Sum
99.90
SiO-.
Undecomposed (Sesquioxide of iron 3.29
by I Alumina .... 8.81
Hydrochloric acid I Magnesia. . . Traces
44.4:1 per cent. |güica ^ and lmd|, 32.33
99.90
Constituents of Sample: —
FeO Fe203 A1203 CaO MgO
0.92 7.24 13.52 0.42 1.94
Loss by Ignition
2.35 = 99-.90.
CaC03 Ps03 SiOs
41.18 Traces 32.33
Station 395.
Station St95.
N. B. 71° 59’. 0. L. 11" 40’. 1110 Favne (2030
Meter). — 1.3°. Lysbrunt Biloculinler. Ingen Stene.
(Som det underste Lag af Bundprøven fandtes noget graat
Ler). Mange Foraminiferer. men forholdsvis laa
Globige-riner. væsentlig Lituola og. Nonionhm.
Dekomponeret
af
Saltsyre
.-1S.79 pCt.
U dekomponeret
af
Saltsyre
42.90 pCt.
Lat. 71° 59’ X.. long. 11" 40’.E.; 1110 fathoms (2030
metres); bottom-temperature — 1.3°. Light-brown
Biloculina clay (on a thin under layer of grey clay) containing a
great many Foraniinifera. but comparatively few
Globige-rituB, belonging in greater part to the genera Lituola and
Nonionma.
Decomposed
by
Hydrochloric acid
02.79 per cent.
Undecomposed
by
Hydrochloric acii]
42.!Mi per cent.
Glødningstab . . 5.27
Jernoxydul. . . 1.26
Jernoxyd . . . 3.57
Lerjord .... 9.19
Kalk.....0.92
Magnesia . . . 0.88
Kulsur Kalk . . 27.09
Fosforsyre . - . Spor
Kiselsyre. . . . 9.88
Jernoxyd ... 1.91
Lerjord .... 10.33
Magnesia . . . 0.80
Kiselsyre . . . 29.92
Sum 101.02
Samlede Bestanddele:
FeO Fe203 A1203 CaO MgO CaC03 PaO„ SiO»
1.26 5.48 19.52 0.92 1.68 27.09 Spor 39.80
Glodn.tab Sum
5.27 101.02.
Station 301.
X. B. 74» l’, V. L. 1° 20’. 1684 Favne (3080
Meter). —1.6°. Biloculinler, mørkere brunt end det
foregaaende. (En ubetydelig Mængde graat Underler).
Forholdsvis faa Foraminiferer.
Loss by ignition . 5.27
Protoxide of iron 1.26
Sesquioxide of iron 3.57
Alumina . . . 9.19
Lime.....0.92
Magnesia . . . 0.88
Carbonate of lime 27 09
Phosphoric acid Traces
Silica.....9.88
f Sesquioxide of iron 1.91
Alumina . . . 10.33
Magnesia . . . O.8O
Silica.....29.92
101.02
Constituents of Sample: —
FeO Fe203 ALOj CaO MgO CaC03 P.OD SiO,.
1.26 5.48 19 52 0.92 1.68 27.09 Traces 39.80
Loss by Ignition
5.27 = 101.02.
Station 301.
Lat. 74° 1’ N., long. 1" 20’ W.; 1684 fathoms (3080
metres); bottom-temperature — 1.6°. Biloculina clay of a
darker brown than the foregoing sample, with a little grey
clay in the under part; comparatively few Foraniinifera.
<< prev. page << föreg. sida << >> nästa sida >> next page >>