台湾岛和黄岩岛的来源研究

Study on the Origin of Taiwan and Huangyan Island

基于特提斯构造演化和东南亚地块的逃逸构造理论,首先论证了东南亚众多地块被从中国青藏高原东南角挤出的必然性。然后从地理形状、山脉走向对台湾岛从菲律宾分离前的状态进行了复原,发现其吻合非常好。同时从地质、地球物理、考古和雅美人的特征分别找到了台湾岛分离的确凿证据。最后证明包括菲律宾、马来西亚、印尼等众多东南亚国家都是随着印度板块的向北挤压从中国青藏高原的东南角被挤出去,并漂移到当前位置。他们大多数是印度板块从特提斯洋底刮蹭下来的堆积岛。台湾岛最后是从吕宋岛分离而来,而黄岩岛是古华夏板块向北漂移过程中在南中国海的产物。

At first based on the Tethyan tectonic evolution and escape tectonics theory about Southeast Asia block, we find it is necessary for the Southeast Asian blocks to extrude from the southeast corner of the Ti-betan Plateau of China. And then we recover the original shape of Taiwan Island before its separation from Philippines. The recovered result show that the geographic shape, mountains direction all fit very well. At the same time, from the characteristics of geological, geophysical, archaeological and Yami people, we find clear separation evidence of Taiwan Island. Finally, we certify that most Southeast Asian countries including Phil-ippines, Malaysia, Indonesia and so on are all the result of the India Plate northward extrusion from China Qinghai-Tibet Plateau. They are the results of squeezed out materials. Most of them are accumulated island scraped down by the India Plate from the Tethys Ocean. Taiwan Island is from Luzon Island with its last sta-tion. Huangyan Island is the drifting product of the ancient Huaxia plate.