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Cambridge University Press (88)
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1950-1954 (88)
1952 (88)
Geological Magazine. 1952; 89(1): 1-21. Published 1952 Feb 01. doi: 10.1017/s0016756800067261. (1)
Geological Magazine. 1952; 89(1): 22-24. Published 1952 Feb 01. doi: 10.1017/s0016756800067273. (1)
Geological Magazine. 1952; 89(1): 25-38. Published 1952 Feb 01. doi: 10.1017/s0016756800067285. (1)
Geological Magazine. 1952; 89(1): 39-40. Published 1952 Feb 01. doi: 10.1017/s0016756800067297. (1)
Geological Magazine. 1952; 89(1): 41-48. Published 1952 Feb 01. doi: 10.1017/s0016756800067303. (1)
Geological Magazine. 1952; 89(1): 49-60. Published 1952 Feb 01. doi: 10.1017/s0016756800067315. (1)
Geological Magazine. 1952; 89(1): 61-69. Published 1952 Feb 01. doi: 10.1017/s0016756800067327. (1)
Geological Magazine. 1952; 89(1): 69-70. Published 1952 Feb 01. doi: 10.1017/s0016756800067339. (1)
Geological Magazine. 1952; 89(1): 70-70. Published 1952 Feb 01. doi: 10.1017/s0016756800067340. (1)
Geological Magazine. 1952; 89(1): 71-71. Published 1952 Feb 01. doi: 10.1017/s0016756800067352. (1)
Geological Magazine. 1952; 89(1): 71-72. Published 1952 Feb 01. doi: 10.1017/s0016756800067364. (1)
Geological Magazine. 1952; 89(1): 72-72. Published 1952 Feb 01. doi: 10.1017/s0016756800067376. (1)
Geological Magazine. 1952; 89(1): 72-72. Published 1952 Feb 01. doi: 10.1017/s0016756800067388. (1)
Geological Magazine. 1952; 89(2): 106-112. Published 1952 Apr 01. doi: 10.1017/s0016756800067443. (1)
Geological Magazine. 1952; 89(2): 113-123. Published 1952 Apr 01. doi: 10.1017/s0016756800067455. (1)
Geological Magazine. 1952; 89(2): 124-128. Published 1952 Apr 01. doi: 10.1017/s0016756800067467. (1)
Geological Magazine. 1952; 89(2): 129-140. Published 1952 Apr 01. doi: 10.1017/s0016756800067479. (1)
Geological Magazine. 1952; 89(2): 141-144. Published 1952 Apr 01. doi: 10.1017/s0016756800067480. (1)
Geological Magazine. 1952; 89(2): 145-147. Published 1952 Apr 01. doi: 10.1017/s0016756800067492. (1)
Geological Magazine. 1952; 89(2): 148-151. Published 1952 Apr 01. doi: 10.1017/s0016756800067509. (1)
2106

Zeitschrift

Geological Magazine. 1952; 89(1): 1-21. Published 1952 Feb 01. doi: 10.1017/s0016756800067261. (1)
Geological Magazine. 1952; 89(1): 22-24. Published 1952 Feb 01. doi: 10.1017/s0016756800067273. (1)
Geological Magazine. 1952; 89(1): 25-38. Published 1952 Feb 01. doi: 10.1017/s0016756800067285. (1)
Geological Magazine. 1952; 89(1): 39-40. Published 1952 Feb 01. doi: 10.1017/s0016756800067297. (1)
Geological Magazine. 1952; 89(1): 41-48. Published 1952 Feb 01. doi: 10.1017/s0016756800067303. (1)

Geological Magazine. 1952; 89(1): 49-60. Published 1952 Feb 01. doi: 10.1017/s0016756800067315. (1)

Geological Magazine. 1952; 89(1): 61-69. Published 1952 Feb 01. doi: 10.1017/s0016756800067327. (1)

Geological Magazine. 1952; 89(1): 69-70. Published 1952 Feb 01. doi: 10.1017/s0016756800067339. (1)

Geological Magazine. 1952; 89(1): 70-70. Published 1952 Feb 01. doi: 10.1017/s0016756800067340. (1)

Geological Magazine. 1952; 89(1): 71-71. Published 1952 Feb 01. doi: 10.1017/s0016756800067352. (1)

Geological Magazine. 1952; 89(1): 71-72. Published 1952 Feb 01. doi: 10.1017/s0016756800067364. (1)

Geological Magazine. 1952; 89(1): 72-72. Published 1952 Feb 01. doi: 10.1017/s0016756800067376. (1)

Geological Magazine. 1952; 89(1): 72-72. Published 1952 Feb 01. doi: 10.1017/s0016756800067388. (1)

Geological Magazine. 1952; 89(2): 106-112. Published 1952 Apr 01. doi: 10.1017/s0016756800067443. (1)

Geological Magazine. 1952; 89(2): 113-123. Published 1952 Apr 01. doi: 10.1017/s0016756800067455. (1)

Geological Magazine. 1952; 89(2): 124-128. Published 1952 Apr 01. doi: 10.1017/s0016756800067467. (1)

Geological Magazine. 1952; 89(2): 129-140. Published 1952 Apr 01. doi: 10.1017/s0016756800067479. (1)

Geological Magazine. 1952; 89(2): 141-144. Published 1952 Apr 01. doi: 10.1017/s0016756800067480. (1)

Geological Magazine. 1952; 89(2): 145-147. Published 1952 Apr 01. doi: 10.1017/s0016756800067492. (1)

Geological Magazine. 1952; 89(2): 148-151. Published 1952 Apr 01. doi: 10.1017/s0016756800067509. (1)

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A Palaeogeographical Atlas of the British Isles and adjacent parts of Europe. By Leonard J. Wills. pp. 64, with 12 plates containing 54 maps. 11 x 8½ inches. London and Glasgow: Blackie and Son, Ltd., 1951. Price 21s. (1952)

M. B.,

Cambridge University Press

In: Geological Magazine. 1952; 89(6): 441-442. Published 1952 Dec 01. doi: 10.1017/s0016756800068199.

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Publikationsdatum: 1952-12-01

Print ISSN: 0016-7568

Digitale ISSN: 1469-5081

Thema: Geologie und Paläontologie

Publiziert von Cambridge University Press

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Foraminiferal Zones in the Tertiary of Australia (1952)

Raggatt, H. G.

Cambridge University Press

In: Geological Magazine. 1952; 89(6): 437-438. Published 1952 Dec 01. doi: 10.1017/s001675680006814x.

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Publikationsdatum: 1952-12-01

Print ISSN: 0016-7568

Digitale ISSN: 1469-5081

Thema: Geologie und Paläontologie

Publiziert von Cambridge University Press

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The Position of the Falkland Islands in a Reconstruction of Gondwanaland (1952)

Adie, Raymond J.

Cambridge University Press

In: Geological Magazine. 1952; 89(6): 401-410. Published 1952 Dec 01. doi: 10.1017/s0016756800068102.

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Publikationsdatum: 1952-12-01

Beschreibung: In previous reconstructions of Gondwanaland the Falkland Islands have been placed in a position intermediate between the Cape Province and Northern Argentina. In the present paper it is suggested on structural, tectonic, and stratigraphical grounds that it would be preferable to position the Falkland Islands due east of the Eastern Province coast, thus completing the truncated Karroo Basin, the missing part of which has until now been suspected to be concealed beneath the ice-capped Queen Maud Land, Antarctica.

Print ISSN: 0016-7568

Digitale ISSN: 1469-5081

Thema: Geologie und Paläontologie

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List of Publications Received (1952)

Cambridge University Press

In: Geological Magazine. 1952; 89(6): 443-444. Published 1952 Dec 01. doi: 10.1017/s0016756800068229.

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Publikationsdatum: 1952-12-01

Print ISSN: 0016-7568

Digitale ISSN: 1469-5081

Thema: Geologie und Paläontologie

Publiziert von Cambridge University Press

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Limestone Blocks in the Lower Cretaceous Cuche Formation of the Central Range, Trinidad, B.W.I. (1952)

Barr, K. W.

Cambridge University Press

In: Geological Magazine. 1952; 89(6): 417-425. Published 1952 Dec 01. doi: 10.1017/s0016756800068126.

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Publikationsdatum: 1952-12-01

Beschreibung: The occurrence of large blocks of fossiliferous Cretaceous limestone among the Lower Cretaceous shales of the Central Range area of Trinidad, B.W.I., has been known for many years, and several different modes of origin have been advanced. A critical exposure which shows the field relationships between the shales and limestone blocks is described, from which it is concluded that the limestone blocks were derived from the contemporaneous breaking up of limestone reefs, and the inclusion of such blocks, together with fore-reef breccia, in the adjacent shale deposits.

Print ISSN: 0016-7568

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Thema: Geologie und Paläontologie

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The Cove Marine Bands (1952)

Anderson, W.

Cambridge University Press

In: Geological Magazine. 1952; 89(6): 440-440. Published 1952 Dec 01. doi: 10.1017/s0016756800068175.

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Publikationsdatum: 1952-12-01

Print ISSN: 0016-7568

Digitale ISSN: 1469-5081

Thema: Geologie und Paläontologie

Publiziert von Cambridge University Press

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Mugearites and Oligoclase-Basalts (1952)

MacGregor, A. G.

Cambridge University Press

In: Geological Magazine. 1952; 89(6): 439-439. Published 1952 Dec 01. doi: 10.1017/s0016756800068163.

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Publikationsdatum: 1952-12-01

Print ISSN: 0016-7568

Digitale ISSN: 1469-5081

Thema: Geologie und Paläontologie

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Fossil Lineages and Environmental Change (1952)

Joysey, Kenneth A.

Cambridge University Press

In: Geological Magazine. 1952; 89(5): 357-360. Published 1952 Oct 01. doi: 10.1017/s0016756800067959.

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Publikationsdatum: 1952-10-01

Beschreibung: An attempt is made to correlate the concept of the fossil lineage with our knowledge of polytypic species. The influence of changing environmental conditions in the geological succession and the relationship between geographical and chronological sub-species is analysed on a theoretical basis. The fossil lineage is considered to be the resultant of combined evolutionary and environmental change. Phenotypic modifications in response to environmental conditions are discussed in relation to the study of variation in fossil communities.

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Thema: Geologie und Paläontologie

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The Cove Marine Bands in East Lothian and their Relation to the Ironstone Shale and Limestone of Redesdale, Northumberland (1952)

Wilson, H. Hugh

Cambridge University Press

In: Geological Magazine. 1952; 89(5): 305-319. Published 1952 Oct 01. doi: 10.1017/s001675680006790x.

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Publikationsdatum: 1952-10-01

Beschreibung: Study of the fauna from a newly discovered fossiliferous outcrop of the Cove Lower Marine Band in Thornton Burn, East Lothian, has led to the correlation of this horizon with the Redesdale Ironstone in Northumberland and has thereby demonstrated the first palaeontological link between the Upper Calciferous Sandstone in S.E. Scotland and the Lower Limestone Group in N.E. England. The collection of D1 fauna made from the Thornton Burn outcrop includes goniatites, brachiopods, lamellibranchs, and crinoids. The discovery of Beyrichoceratoides redesdalensis (Hind) gives the first definite indication of the presence of B zone in the Scottish Carboniferous. Faunal lists and descriptions of some of the more interesting species are included in this paper as well as descriptions of the crinoids collected which are given in the succeeding paper by James Wright.

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Thema: Geologie und Paläontologie

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New Evidence on the Correlation of the Lower Carboniferous Reefs at Castleton, North Derbyshire (1952)

Ford, Trevor D.

Cambridge University Press

In: Geological Magazine. 1952; 89(5): 346-356. Published 1952 Oct 01. doi: 10.1017/s0016756800067947.

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Publikationsdatum: 1952-10-01

Beschreibung: There are two alternative hypotheses regarding the relationship of the goniatite-bearing reef limestones to the coral-bearing “massif” limestones. One claims an unconformity between the reefs and bedded limestones, the other a lateral passage from a “massif facies” to “marginal facies”. Surface exposures are such that it is difficult to be convinced of either hypothesis. Details of underground exposures in natural cave systems and associated mine-workings show a clear transition between facies and no trace of unconformity.

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Thema: Geologie und Paläontologie

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