| 1. |
Proceedings of the Seventh Annual Meeting Held in Peiping, March 29‐31, 1930. |
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Bulletin of the Geological Society of China,
Volume 9,
Issue 1,
1930,
Page 1-5
K H. Hsu,
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ISSN:1673-274X
DOI:10.1111/j.1755-6724.1930.mp9001001.x
出版商:Geological Publishing House
年代:1930
数据来源: WILEY
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| 2. |
Interim Report on the Skull of Sinanthropus* |
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Bulletin of the Geological Society of China,
Volume 9,
Issue 1,
1930,
Page 7-10
Davidson Black,
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ISSN:1673-274X
DOI:10.1111/j.1755-6724.1930.mp9001002.x
出版商:Geological Publishing House
年代:1930
数据来源: WILEY
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| 3. |
Geological Observations in Northern Manchuria and Barga (Hailar). |
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Bulletin of the Geological Society of China,
Volume 9,
Issue 1,
1930,
Page 23-35
E. Licent,
P. Teilhard De Chardin,
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ISSN:1673-274X
DOI:10.1111/j.1755-6724.1930.mp9001003.x
出版商:Geological Publishing House
年代:1930
数据来源: WILEY
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| 4. |
Note on the Chihsia Limestone and its Associated Formation |
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Bulletin of the Geological Society of China,
Volume 9,
Issue 1,
1930,
Page 37-43
J. S. Lee,
S. Chu,
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ISSN:1673-274X
DOI:10.1111/j.1755-6724.1930.mp9001004.x
出版商:Geological Publishing House
年代:1930
数据来源: WILEY
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| 5. |
The Paote and Chingshui Physiographic Stages and their Significance. |
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Bulletin of the Geological Society of China,
Volume 9,
Issue 1,
1930,
Page 45-48
George B. Barbour,
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ISSN:1673-274X
DOI:10.1111/j.1755-6724.1930.mp9001005.x
出版商:Geological Publishing House
年代:1930
数据来源: WILEY
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| 6. |
Further Data Regarding Deep Wells in the Peking Area. |
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Bulletin of the Geological Society of China,
Volume 9,
Issue 1,
1930,
Page 49-57
George B. Barbour,
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ISSN:1673-274X
DOI:10.1111/j.1755-6724.1930.mp9001006.x
出版商:Geological Publishing House
年代:1930
数据来源: WILEY
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| 7. |
The Structure of Sacred Omeishan, Szechuan |
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Bulletin of the Geological Society of China,
Volume 9,
Issue 1,
1930,
Page 59-75
Arnold Heim,
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ISSN:1673-274X
DOI:10.1111/j.1755-6724.1930.mp9001007.x
出版商:Geological Publishing House
年代:1930
数据来源: WILEY
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| 8. |
The Geology in Eastern Shantung* |
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Bulletin of the Geological Society of China,
Volume 9,
Issue 1,
1930,
Page 79-91
H. S. Wang,
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摘要:
SUMMARYFollowing the deposition of Wutai formation, there occured a period of intense disturbance accompanied by igneous intrusion through which the Wutai formation has been strongly folded and metamorphosed. Since then ensued a long period of erosion until Mesozoic time when the folded mountains were completely reduced to a peneplane. It was due to subsequent warping and faulting of this old peneplaned surface that came into existence the Laiyang basin which extended at that time in NE‐SW direction. So far as the present exposures are concerned, it began from Tieh Kou Tsion the northeast and thence southwestward through the Lai Yang city to Chang Ying of Chiao Hsien on the southwest. Like most of the Mesozoic basins in other parts of the country, its sediments including the fossils as well were of a continental type, accumulated probably under a dominantly moist and warm climate. The rocks composing the floor are usually of the very ancient type, ranging from Archaean to Algonkian; they are as a rule rather complicated in structure. The Laiyang basin was then closed by the explosion of the Ching Shan volcanics which were in turn succeeded by the Wangshih series, the last record in Mesozoic time. After the deposition of the last Cretaceous sediment, warping as well as faulting became active again in Tertiary time. Some of them are still very conspicuous in the present topographical feature
ISSN:1673-274X
DOI:10.1111/j.1755-6724.1930.mp9001008.x
出版商:Geological Publishing House
年代:1930
数据来源: WILEY
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| 9. |
Preliminary Note on an Occurrence of Late Palæozoic Tillite in the Kuruk‐Tagh Mountains, Sinkiang, China.* |
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Bulletin of the Geological Society of China,
Volume 9,
Issue 1,
1930,
Page 93-94
Erik Norin,
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ISSN:1673-274X
DOI:10.1111/j.1755-6724.1930.mp9001009.x
出版商:Geological Publishing House
年代:1930
数据来源: WILEY
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Volume 9 issue 1