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多地理指标限定的奥陶纪-泥盆纪华南古地理位置重建模型
杨晨, 景先庆
PDF(2404 KB)
PDF(2404 KB)
多地理指标限定的奥陶纪-泥盆纪华南古地理位置重建模型
华南板块有丰富的古生代生物重大演化事件的地层记录，因而是研究古地理环境变化与生物演化的天然实验室.但这一时期华南的古地理位置存在较大争议.综合利用古地磁、古生物演化事件、古地理环境变化等指标，对古生代中期华南板块不同古地理重建模型进行评价.表明现有模型很难吻合以上大多数指标.基于奥陶纪末期真极移事件以及古地磁结果，我们建立了奥陶纪末‒泥盆纪4个不同时期的华南古地理重建新模型.该模型表明华南与冈瓦那大陆的关系是动态的，具有从近到远又由远及近的运动过程.此模型可以很好地吻合华南现有古生物、古地磁及古地理环境变化等数据，为后期研究古生代地理环境与生物演化的关系提供了更准确的古地理重建基础.
South China Block is a natural laboratory for the study of paleogeographic environmental changes and biological evolution since it has myriad records of major biological evolutionary events in the Paleozoic. However, the paleogeographic location of South China during this period remains controversial. In this paper it selects and evaluates different paleogeographic reconstruction models of the South China Block in the Middle Paleozoic by using of the paleomagnetic data, paleontological evolution pattern, paleogeographic environmental changes and other indicators. It is difficult for the existing models to match most of these indicators. On the basis of the newly proposed paleogeographic reconstruction of South China at the end of Ordovician based on true polar wandering, it established the paleogeographic location model of South China at four different periods from the Late Ordovician to Devonian. The model shows that the relationship between South China and the Gondwana is dynamically evolving, with a movement from near to far and from far to near. Moreover, this model can well match the existing data of paleomagnetism, paleontology, tectonic evolution and paleogeographic environment changes in South China, which provides a high accuracy paleogeographic reconstruction for the further study of the Paleozoic environment and paleontological evolution in South China.
古生代中期 / 华南 / 古地理重建 / 生物演化 / 环境地质.
Middle Paleozoic / South China / paleogeographic reconstruction / biological evolution / environmental geology
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