晚古生代－三叠纪南盘江海的构造古地理问题

doi:10.7605/gdlxb.2003.01.006

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Abstract

From Devonian to Triassic the Nanpanjiang Sea developed in Yunnan, Guizhou and Guangxi in China and their adjacent area in northern Vietnam. Geologically, there were the Yangtze Block on its north, the Yunkai Block and Damingshan Block on its southeast and the North Vietnam Block on its southwest. Within the Nanpanjiang Sea the Tianlin Basin located on its northern part, the Babu Basin with oceanic crust on its central part and the Qinfang Basin on its southern part. It also contains a lot of submarine platform with different size, of which the largest was the Damingshan Platform, secondly were the Jingxi Platform and the Xichou Platform. The opening of the Nanpanjiang Sea at later Early Devonian might be the result that the counter-clockwise rotation of the Gandwanaland and the northward drift of the Yangtze Block caused the rifting of the Guangxi-Yunnan-North Vietnam Block among them at that time. Further sea-floor spreading led to the occurrence of oceanic crust in Babu Basin and the Nanpanjiang Sea exceeded beyond 20 latitudes from north to south in Early Carboniferous. The oceanic spreading ridge might link with that in Ailaoshan Sea to the west based on the paleogeographic reconstruction. During Late Permian the Yunkai Block drifted northward and collided with the Damingshan Block. Then the Indosinian Block moved northward and amalgamated with North Vietnam Block in early Triassic. An active margin appeared in the southern border of the Nanpanjiang Sea from Late Permian to Middle Triassic. In Late Triassic the Indosinian - North Vietnam Block amalgamated with the Yangtze Block and the Nanpanjiang Sea closed. The opening, developing and closing of the Nanpanjiang Sea, Ailaoshan Sea and Changning-Menglian Sea were basically kept the same pace. Those marine basins might be controlled by the same oceanic ridge system of the Paleo-Tethys.

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Published: 01 February 2003

About author: Wu Haoruo, born in 1940, graduated from the Beijing College of Geology in 1962. Now he is a professor of the Institute of Geology and Geophysics, Chinese Academy of Sciences, and engages in paleontology and stratigraphy.

Cite this article:

. A DISCUSSION ON THE TECTONIC PALAEOGEOGRAPHY OF THE NANPANJIANG SEA IN LATE PALAEOZOIC AND TRIASSIC[J]. JOURNAL OF PALAEOGEOGRAPHY, 2003, 5(1): 63-76.

. A DISCUSSION ON THE TECTONIC PALAEOGEOGRAPHY OF THE NANPANJIANG SEA IN LATE PALAEOZOIC AND TRIASSIC[J]. JOPC, 2003, 5(1): 63-76.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2003.01.006 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2003/V5/I1/63

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