1. |
Korrespnderande ledamöter |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 3-16
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ISSN:0016-786X
DOI:10.1080/11035895709449108
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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2. |
Geologiska föreningen sänder sina förhandlingar såsom publikationsutbyte till följande sällskap, institutioner etc. i utlandet |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 17-20
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ISSN:0016-786X
DOI:10.1080/11035895709449109
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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3. |
Notes on the Upper Ordovician and Lower Silurian of the Tapa District, Estonia |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 21-34
Jüri Martna,
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摘要:
The Upper Ordovician Saunja (Fia), Vormsi (Fib), Pirgu (Fic), and Porkuni (F2; in this paper included in the Ordovician) stages and the Lower Silurian Juuru (G1) stage are briefly characterized lithologically and faunistically according to the writer's field observations in the Tapa district. A stratigraphic column of the Lower Silurian in central Estonia up to the Adavere (H) stage is republished, somewhat modified, after Elsa Rosenstein (1943). A correlation of the lowermost Silurian between Estonia and Norway is suggested, whereby the supposedly considerable hiatus between the Porkuni and Juuru stages is much diminished.
ISSN:0016-786X
DOI:10.1080/11035895709449110
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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4. |
Some Data concerning the Mineralogy of the Karlshamn Granite |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 35-42
RolfB. Norin,
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摘要:
The granite, a coarse massive type, contains the following minerals: quarz, microcline, oligoclase, biotite, sphene, apatite, zircon, and magnetite with some secondary sericite, chlorite, and calcite. The minerals were isolated according to the method shown diagrammatically in Fig. 1. The relation between chemical composition and optical properties of the microcline and the biotite is elucidated. In the system of P. Niggli the granite represents a normal-granitic to yosemite-granitic magma type.
ISSN:0016-786X
DOI:10.1080/11035895709449111
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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5. |
Determination of the Composition of Garnets without Chemical Analysis |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 43-51
Rudyard Frietsch,
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摘要:
In the present paper an account is given of the extent a determination of only the unit cell dimension and the refractive index may be used to predicte the composition of a garnet. For this purpose 17 analysed garnets were investigated, the unit cell dimensions and the refractive indices are shown in Table 1. By using fig. 1 and 2, in which the unit cell size and the refractive index of 60 analysed garnets have been combined, it is possible to obtain a characterization accurate enough to be used in petrogenetical problems. To distinguish accurately between an almandite and a spessartite partial chemical analysis for manganese is necessary. From fig. 2 it seems clear, however, that a garnet with n > 1.80 and < 1.82 is not especially rich in spessartite.
ISSN:0016-786X
DOI:10.1080/11035895709449112
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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6. |
The Clay Minerals in the Ordovician Bentonite Beds in Billingen, Southwest Sweden |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 52-56
AnnMarie Byström,
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摘要:
A preliminary investigation has been made of the bentonite beds in Billingen, Vestergötland, Sweden. The clay consists of a complex mixed layer mineral; the layers are mostly illitic and are mixed with probably chloritic and partly dehydrated montmorillonite layers. This clay mineral differs from the types found in the corresponding beds at Kinnekulle, 30 km, NW of Billingen, but is similar to the clay mineral found in the K-bentonites of Pennsylvania. Chlorite is present in varying amounts.
ISSN:0016-786X
DOI:10.1080/11035895709449113
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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7. |
Meddelande från Svenska Föreningen För Lerforskning (Reports of Swedish Clay Research |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 57-57
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ISSN:0016-786X
DOI:10.1080/11035895709449114
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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8. |
Hydration and hydroxylation with special reference to montmorillonite |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 58-61
RobertC. Mackenzie,
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ISSN:0016-786X
DOI:10.1080/11035895709449115
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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9. |
Om finska kvartära lerors mineralproblematik |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 62-66
U. Soveri,
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摘要:
The mineralogical composition of Finnish Pleistocene sediments is discussed and the rôle of geological factors is denoted.
ISSN:0016-786X
DOI:10.1080/11035895709449116
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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10. |
Om apparatfrågan vid automatisk granulometrisk analys |
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Geologiska Föreningen i Stockholm Förhandlingar,
Volume 79,
Issue 1,
1957,
Page 66-69
T. Hagerman,
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摘要:
For measurement and statistical investigation of such properties as the parameters, surface and shape of the projection of fine particles and pores respectively in the section of a solid, automatic instrument is required which can be further developed. On proposal of the author design work for such an instrument limited to measurements of the length and width of sediment particles has been carried out for several years at the Royal Institute of Technology, Division of Electrical measurements. The system of an electronic investigator including a television tube for analysing and a computing machine is recommended. Provided that it will be possible to apply the instrument to a great many fields the development and completion thereof should interest not only researchers but various industries as well.
ISSN:0016-786X
DOI:10.1080/11035895709449117
出版商:Taylor & Francis Group
年代:1957
数据来源: Taylor
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