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| 1. |
Proceedings of the Third Annual Meeting of the Geological Society of China, Held in Pfking, January 3,4, and 5, 1925. |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 1-14
Y. C. Sun,
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PDF (259KB)
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ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001001.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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| 2. |
Geological Notes from Kansu |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 15-18
J. G. Andersson,
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PDF (93KB)
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摘要:
(Abstract)The specimen is collected from a small outcrop near the Lolo village of Mao Mao Kou, some 30 km. N.N.W. of Hui Li district in S. Szechuan, on the N. slope of Lung Tsao Shan, a prominant mountain some 8,000 feet above the sea, entirely covered by a basaltic lava of Permian age. The latter weathers into a residual red clay which covers the lower slopes. The contact of the syenite with the Lung Tsao Shan lava was not observed owing to the thick cover. East of the occurrence a series of steep dipping red shales appears. The exact relation of this series with the syenite is not clear, but it is probable that they are in actual contact. Further east the red shale series is thrown into contact with a coal series containing Rhætic plant fossils—probably by an overthrust as the whole coal series is highly fold
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001002.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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| 3. |
The Ordovician Graptolite Beds of Ping Liang, E. Kansu |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 19-20
P. L. Yuan,
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PDF (59KB)
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摘要:
(Abstract)The specimen is collected from a small outcrop near the Lolo village of Mao Mao Kou, some 30 km. N.N.W. of Hui Li district in S. Szechuan, on the N. slope of Lung Tsao Shan, a prominant mountain some 8,000 feet above the sea, entirely covered by a basaltic lava of Permian age. The latter weathers into a residual red clay which covers the lower slopes. The contact of the syenite with the Lung Tsao Shan lava was not observed owing to the thick cover. East of the occurrence a series of steep dipping red shales appears. The exact relation of this series with the syenite is not clear, but it is probable that they are in actual contact. Further east the red shale series is thrown into contact with a coal series containing Rhætic plant fossils—probably by an overthrust as the whole coal series is highly fold
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001003.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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| 4. |
Geological Notes on Eastern Kansu§ |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 21-28
Preview
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PDF (197KB)
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摘要:
(Abstract)The specimen is collected from a small outcrop near the Lolo village of Mao Mao Kou, some 30 km. N.N.W. of Hui Li district in S. Szechuan, on the N. slope of Lung Tsao Shan, a prominant mountain some 8,000 feet above the sea, entirely covered by a basaltic lava of Permian age. The latter weathers into a residual red clay which covers the lower slopes. The contact of the syenite with the Lung Tsao Shan lava was not observed owing to the thick cover. East of the occurrence a series of steep dipping red shales appears. The exact relation of this series with the syenite is not clear, but it is probable that they are in actual contact. Further east the red shale series is thrown into contact with a coal series containing Rhætic plant fossils—probably by an overthrust as the whole coal series is highly fold
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001004.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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| 5. |
Carboniferous Stratigraphy of Northwestern Kansu.§ |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 29-37
P. L. Yuan,
Preview
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PDF (187KB)
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摘要:
(Abstract)The specimen is collected from a small outcrop near the Lolo village of Mao Mao Kou, some 30 km. N.N.W. of Hui Li district in S. Szechuan, on the N. slope of Lung Tsao Shan, a prominant mountain some 8,000 feet above the sea, entirely covered by a basaltic lava of Permian age. The latter weathers into a residual red clay which covers the lower slopes. The contact of the syenite with the Lung Tsao Shan lava was not observed owing to the thick cover. East of the occurrence a series of steep dipping red shales appears. The exact relation of this series with the syenite is not clear, but it is probable that they are in actual contact. Further east the red shale series is thrown into contact with a coal series containing Rhætic plant fossils—probably by an overthrust as the whole coal series is highly fold
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001005.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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| 6. |
A Study of the Silurian Section at Lo Jo Ping, I Chang District, W. Hupeh§ |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 39-44
C. Y. Hsieh,
Y. T. Chao,
Preview
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PDF (126KB)
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摘要:
(Abstract)The specimen is collected from a small outcrop near the Lolo village of Mao Mao Kou, some 30 km. N.N.W. of Hui Li district in S. Szechuan, on the N. slope of Lung Tsao Shan, a prominant mountain some 8,000 feet above the sea, entirely covered by a basaltic lava of Permian age. The latter weathers into a residual red clay which covers the lower slopes. The contact of the syenite with the Lung Tsao Shan lava was not observed owing to the thick cover. East of the occurrence a series of steep dipping red shales appears. The exact relation of this series with the syenite is not clear, but it is probable that they are in actual contact. Further east the red shale series is thrown into contact with a coal series containing Rhætic plant fossils—probably by an overthrust as the whole coal series is highly fold
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001006.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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| 7. |
The Mesozoic Stratigraphy of the Yangtze Gorges.§ |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 45-51
C. Y. Hsieh,
Y. T. Chao,
Preview
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PDF (152KB)
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摘要:
(Abstract)The specimen is collected from a small outcrop near the Lolo village of Mao Mao Kou, some 30 km. N.N.W. of Hui Li district in S. Szechuan, on the N. slope of Lung Tsao Shan, a prominant mountain some 8,000 feet above the sea, entirely covered by a basaltic lava of Permian age. The latter weathers into a residual red clay which covers the lower slopes. The contact of the syenite with the Lung Tsao Shan lava was not observed owing to the thick cover. East of the occurrence a series of steep dipping red shales appears. The exact relation of this series with the syenite is not clear, but it is probable that they are in actual contact. Further east the red shale series is thrown into contact with a coal series containing Rhætic plant fossils—probably by an overthrust as the whole coal series is highly fold
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001007.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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| 8. |
The Deposits of the Sang Kan Ho Valley |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 53-55
G. B. Barbour,
Preview
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PDF (92KB)
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摘要:
(Abstract)The specimen is collected from a small outcrop near the Lolo village of Mao Mao Kou, some 30 km. N.N.W. of Hui Li district in S. Szechuan, on the N. slope of Lung Tsao Shan, a prominant mountain some 8,000 feet above the sea, entirely covered by a basaltic lava of Permian age. The latter weathers into a residual red clay which covers the lower slopes. The contact of the syenite with the Lung Tsao Shan lava was not observed owing to the thick cover. East of the occurrence a series of steep dipping red shales appears. The exact relation of this series with the syenite is not clear, but it is probable that they are in actual contact. Further east the red shale series is thrown into contact with a coal series containing Rhætic plant fossils—probably by an overthrust as the whole coal series is highly fold
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001008.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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| 9. |
On the Stratigraphy of North Shensi |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 57-80
C. C. Wang,
Preview
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PDF (1178KB)
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摘要:
(Abstract)The specimen is collected from a small outcrop near the Lolo village of Mao Mao Kou, some 30 km. N.N.W. of Hui Li district in S. Szechuan, on the N. slope of Lung Tsao Shan, a prominant mountain some 8,000 feet above the sea, entirely covered by a basaltic lava of Permian age. The latter weathers into a residual red clay which covers the lower slopes. The contact of the syenite with the Lung Tsao Shan lava was not observed owing to the thick cover. East of the occurrence a series of steep dipping red shales appears. The exact relation of this series with the syenite is not clear, but it is probable that they are in actual contact. Further east the red shale series is thrown into contact with a coal series containing Rhætic plant fossils—probably by an overthrust as the whole coal series is highly fold
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001009.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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| 10. |
List of New Members |
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Bulletin of the Geological Society of China,
Volume 4,
Issue 1,
1925,
Page 81-81
A. Fellows,
Preview
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PDF (36KB)
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摘要:
(Abstract)The specimen is collected from a small outcrop near the Lolo village of Mao Mao Kou, some 30 km. N.N.W. of Hui Li district in S. Szechuan, on the N. slope of Lung Tsao Shan, a prominant mountain some 8,000 feet above the sea, entirely covered by a basaltic lava of Permian age. The latter weathers into a residual red clay which covers the lower slopes. The contact of the syenite with the Lung Tsao Shan lava was not observed owing to the thick cover. East of the occurrence a series of steep dipping red shales appears. The exact relation of this series with the syenite is not clear, but it is probable that they are in actual contact. Further east the red shale series is thrown into contact with a coal series containing Rhætic plant fossils—probably by an overthrust as the whole coal series is highly fold
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1925.mp4001010.x
出版商:Geological Publishing House
年代:1925
数据来源: WILEY
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