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Based on integrative data of systematics, fossil history, and morphological and molecular evidence of these genera, their origin, evolution and relationships were discussed.
      
Through research on characteristics such as shape, modality and structure of these fossils symbiotic with Punctatus emeiensis, the author found many possible embryo fossils including the evidence of gastrula-stage animal fossils.
      
Evidence of the transgression lake of the Subei basin during Late Cretaceous and Paleocene and its geological significance
      
The evidence of paleontology, minerals in rocks and geochemistry can help confirm the environment of the lake basin that developed during the Late Cretaceous and Paleocene.
      
The defects at anaphase 1 and anaphase 2 did not affect the karyotype constancy and their absence at the tetrad stage can be considered as an evidence of cytological stability of the studied material.
      
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Fossils of "Huainan biota" were first discoverd in Liulaopei formation of Huanain of Huainan Group in sinian of China in 1962. Their main categories are as follows: Chuaridae, Sabelliditidae, Neovendotaenidae, and many othecr fossils the taxonomic position of which is not yet determined. Being of Carbouceous films of millimetric size, these well well preserved biological fossils were soltary of existence , but buried in clusters, occurring in extreme abundance and widely distributed. They have a certain time...

Fossils of "Huainan biota" were first discoverd in Liulaopei formation of Huanain of Huainan Group in sinian of China in 1962. Their main categories are as follows: Chuaridae, Sabelliditidae, Neovendotaenidae, and many othecr fossils the taxonomic position of which is not yet determined. Being of Carbouceous films of millimetric size, these well well preserved biological fossils were soltary of existence , but buried in clusters, occurring in extreme abundance and widely distributed. They have a certain time relation with such strontianites as Gymnosolen Baicalia and such microfossils as Iaminaretas, Taeniotum. Their age is about 850 m.y.This assocciation of the biological fossils can be regarded as one of the biological evidence of the regional stratigraphic comparison.

本文介绍了震旦纪“淮南生物群”的发育和组合特征及其产出状况,初步确定了该生物群繁盛的时限,对以往许多学者曾依据地质历史分析和其他方法进行对比的地层,作了综合分折和比较,进而就“淮南生物群”在地层对比中的可能性进行了探讨。

Basing upon the Landsat images this paper briefly described the active faults in Taiwan province and their relation to the earthquakes. The active faults, elongated mostly in a form of belt with distinct tectonic activity, are clearly characterized by the satellite images. The region under investigation is principally controlled by the NNE trending active fault zones, which usually have a left-lateral character. Although the NW trending active zones are not so large on the scale as the former, they behave as...

Basing upon the Landsat images this paper briefly described the active faults in Taiwan province and their relation to the earthquakes. The active faults, elongated mostly in a form of belt with distinct tectonic activity, are clearly characterized by the satellite images. The region under investigation is principally controlled by the NNE trending active fault zones, which usually have a left-lateral character. Although the NW trending active zones are not so large on the scale as the former, they behave as a fault with evidence of recent movement in northern Taiwan and are right-lateral in nature. By synthetic analysis of data concerned this region is determined to be compressed from NNW-SSE direction, due to the collision between the Phillippine Sea plate and the Eurasian plate.

本文是根据Landsat卫星影像概括分析了台湾岛的活动断裂及其与地震的关系。在卫星影像上,活动断裂的特点是影像清晰,多成带出现,活动性明显。北北东向活动断裂带构成本区的基本轮廓,多数具有左旋平移性质;北西向活动断裂带的规模虽不如前者,但有可能是台湾岛北部最新的活动断裂,并具有右旋平移性质。通过综合分析表明,本区大致承受北北西—南南东方向的挤压作用,即菲律宾海板块与欧亚板块碰撞挤压的结果。

The Hunhe fault zone is a western extension of the Shenyang-Dunhua Mishan fault and there can be found an evidence of Pre-Sinian movement. It is suggested that the faulting of Hunhe fault zone was significant in Mesozoic time and more intensive and frequent in Tertiary and Quaternary.Basing upon the data on geology, morphology and seismicity. this paper illustrates the trace of the neotectonic movement since Tertiary.Actually this fault acts as one of main faults of Cathaysian tectonic system. In general,...

The Hunhe fault zone is a western extension of the Shenyang-Dunhua Mishan fault and there can be found an evidence of Pre-Sinian movement. It is suggested that the faulting of Hunhe fault zone was significant in Mesozoic time and more intensive and frequent in Tertiary and Quaternary.Basing upon the data on geology, morphology and seismicity. this paper illustrates the trace of the neotectonic movement since Tertiary.Actually this fault acts as one of main faults of Cathaysian tectonic system. In general, this paper deals with only the Shenyan-Qingyuan section.

浑河断裂带在前震旦纪就开始活动,中生代时期活动剧烈,至第三纪和第四纪初、浑河断裂带的构造活动更为频繁强烈。本文主要讨论浑河断裂带自沈阳至清原县草市地段从第三纪以来的新构造活动的一些形迹。

 
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