In the course of the application and dissemination , we improve on and perfect all kinds of the technologies according to the original questions existent in image instrument , also we develop the really colorful digital photographic technology , fluorescent digital photographic technology , digital putting pictures together technology , emulsified smear analytical technology and biological stratum evaluated technology ; adducing digital image transaction , image compression , picture and character data - base technology 图像分析处理技术系列的构成、二次开发及其特点；结合石油地质分析的实际情况；对图像处理、图像分析、数字压缩技术和图像拼接技术进行了研究，并在储层评价、生物地层及三次采油研究中的进行了应用，以及讨论了clsm在古生物学领域的应用。
On the basis of extensive field investigations and laboratory analyses on the carboniferous strata and fossils in the west qinling . to the carboniferous of lixian , there has systematically been studied in the lithostratigraphy and biostratigraphy . at the same time , a diverse of fossils form this area have detailedly been described and discussed 在对西秦岭石炭纪地层和古生物化石资料进行广泛的野外收集和室内分析处理的基础上，对研究区石炭系进行了系统的岩石地层和生物地层学的划分和对比；对所获古生物化石进行了系统的描述和归属讨论，形成了一套内容丰富的西秦岭石炭纪地层古生物研究新资料。
This study is a post - cruise study of this leg , calcareous nannofossil samples from sites 1146 , 1147 and 1148 of leg 184 were analyzed to provide a high - resolution biostratigraphy for this leg and to investigate morphological variation of coccolith genus gephyrocapsa . the main results of this study are : 1 . 12 late pliocene to pleistocene bio - events were recognized and 6 zones of martini ( 1971 ) were determined for the upper sediment sequences of sites 1146 and 1148 本文作为大洋钻探项目船下后续研究的一部分，对184航次中的1146站位和1147 、 1148站位的样品进行了分析和研究，在船上科学家已经建立起的地层框架的基础上进一步加密采样，对生物事件标志化石类别进行数量统计，进一步确定了12个生物事件在钻孔中的深度，建立起了两个站位的高分辨率的钙质超微化石生物地层框架。
In addition , these sediments also contain reliable high - resolution paleoenvironmental information both with long - timescale and short - timescale . therefore , this area is an ideal one for the research on the paleoceanography and paleoclimate . for the last decade thermoluminescence ( tl ) has been used for a viable tool for age determination of a variety of rock types and sediments 结合已有丰富的岩芯资料和能代表气候变化的氧同位素地层、碳酸岩地层、生物地层、磁化率地层以及粒度、粘土矿物、色谱等资料，详细开展热释光与古气候变化的对比研究。
Our research work was carried out effectively and fruitfully . this will give exact chronology and sedimentary evidence to the research of the biostratigraphy and thrust slice type stratigraphy of the nongba area ; will provide more full and accurate geological gist for the tectonic evolutions of paleotethyan located in southern part of " three rivers " ; and will provide new reference to the paleolithofacies palaeogeography pattern reconstruction of the changning - menglian oceanic basin 这些工作将为滇西南耿马弄巴地区生物地层学和造山带地层学的研究提供准确的时代和沉积学证据；为“三江”南段古特提斯的构造演化提供更为翔实的地质依据，也为恢复昌宁?孟连洋盆的古地理格架提供了新的参考。
The late ordovician - silurian - devonian - early carboniferous stratigraphic division and correlation , including the chronologic correlation of the donghe sandstone , which are the old great difficult key stratigraphic problems interfering with the development of the oil and gas exploration in the tarim basin , are synthetic studied by systematically applying chemobiostratigraphy . several important relevant stratigraphic boundaries are recognized , and the donghe sandstone is attributed to the frasnian , late devonian . the results of the study in particular proves that chemo - biostratigraphy has great significance and is a practical tool for high resolution stratigraphic division and correlation , especially for the region and or the bed with rare fossils 首次系统应用化学生物地层学对长期遗留的严重阻碍了油气勘探开发步伐的塔里木盆地重大疑难地层问题：晚奥陶世志留纪泥盆纪早石炭世地层划分对比和东河砂岩时代等进行了综合研究，厘定了几条重要的相关地层界线，并将东河砂岩的时代确定为泥盆纪晚泥盆世弗拉斯期。这些研究成果表明，化学生物地层学对高分辨率地层划分对比尤其是对在化石缺乏地区和层段进行地层划分对比工作有重要的意义和实用价值。
There are 25 genera and 47 species of conodont , 4 genera and 6 species of coral and some foraminifera . ch . 4 biostratigraphical regions based on the study on the conodont , coral and foraminifera fossils in research area , it was discovered that the biota features are resemble to the south china . so a conclusion can be drawn that the research area and south china belong to the same biogeographical region 生物地层分区本文通过对牙形刺、蜒类、珊瑚等化石的对比研究，发现研究区的生物群特征与华南区生物群相近，这表明在该区早、晚石炭世与华南区及东古特提斯区同属一个生物地理区系。
