| 1. | Firstly , the lithologic features of bore holes in judian lake ? qingshuibo lake sedimentary area is analyzed , and five typical sections are drawn
首先，分析巨淀湖?清水泊沉积区钻孔中沉积物的岩性特征，绘制5个典型剖面图。 |
| 2. | Through anasynthesis , sum up organic enrichment grading estimating standard of oil source rocks and gas source rocks in our country ( type ii organic matter , mature carbonate rocks )
经过分析综合，归纳出我国碳酸盐岩沉积区(型有机质，成熟碳酸盐岩)气源岩有机质丰度分级评价标准。 |
| 3. | Thirdly , by comparing with holocene strata of the coastal plain of shandong peninsula , sedimentary strata of this area are divided into four layers , and sedimentary environments are comfirmed
再次，通过与山东半岛滨海平原全新统地层进行对比，对本沉积区地层进行划分并确定各层沉积环境。 |
| 4. | The thesis concentrates on judian lakeingshuibo lake sedimentary area which lies in the northern west of shouguang city . by field investigation , the scope of judian lake ? qingshuibo lake is fixed
本次研究将位于寿光市西北部的巨淀湖?清水泊沉积区作为主要研究对象，通过多次野外实地考察和验证，确定了清水泊?巨淀湖的湖区范围。 |
| 5. | By spore - pollen analysis of 10 samples and combining the features of spore - pollen assemblage and climatic environment , the features of evolvement of climatic environment of this sedimentary area since the middle holocene are obtained
本论文还选取其中10个样品进行了孢粉分析，并结合邻近地区的孢粉组合特征和气候环境特征，总结出该沉积区中全新世以来气候环境演变特征。 |
| 6. | The results of the dynamic analysis illuminate that the liquefied area of the dam will be at the top of the coal ash body where coal ash deposits naturally . the depth of the liquefied area is about 20m and the liquefied area is far from the sub - dam , so it does no harm to the dam
该灰坝的动力特性分析表明，灰坝的液化区分布在灰体的上部，主要是在煤灰自然沉积区，液化深度在zom左右，液化区离子坝的距离较远，因此对坝体不构成威胁。 |
| 7. | Member - one of nenjiang group is divided into sa 0 sand - group . the same points of medimentary microfacies types and distribution by developed in many sand groups lies in that they dominate with river delta and shore - shallow lake in west and dominate with deep lake - semi - deep lake and contain gravity flow . the change of sediment scope of each sand - group makes deep lake - semi - deep lake and sublacustrine fan sediment of ga 0 and pu 2 sand - groups not being developed during the lest sediment area , but the deep lake - semi - deep lake and sublacustrine fan sediment during the largest sediment scope of sa 0 is well developed
多数砂组发育的沉积微相类型和分布的共同之处在于，西侧多以河流三角洲和滨浅湖沉积为主，东部以深湖?半深湖为主其中夹有重力流，但由于各砂组沉积范围的变化，造成沉积区最小时期的高0 、葡2砂组深湖?半深湖及湖底扇沉积不发育，而沉积范围最大时期的萨0砂组深湖?半深湖及湖底扇沉积极其发育。 |
| 8. | Finally , through analyzing spore - pollen of 10 samples and consulting the research achievement of the subject , " ancient geographic environmental evolvement on the coastal plain of laizhou bay since holocene " , the features of climatic and environmental changes of this area since the middle holocene are gained
最后，对选取的10个样品进行孢粉分析，并结合“莱州湾滨海平原全新世以来的古地理环境演变”的成果，总结出巨淀湖?清水泊沉积区中全新世以来气候环境变化特征。 |
| 9. | The top sediment above 1 . 8m depth was referred to be the deposit under the cold water mass since 9 . 7kabp . in the middle southern yellow sea . q - mode factor analysis was employed on 98 samples and 33 benthic foraminiferous species with relative abundance of more than 2 % in at least 3 samples and 5 varimax factors had been recognized as follows : factor 1 ( ammonia beccarii vars
南黄海中部泥质区的ey02 - 2孔共揭示了氧同位素6期以来的海侵海退序列，该孔浮游有孔虫匮乏，说明黄海暖流对钻孔所处南黄海中部冷涡泥质沉积区影响一直很弱，底栖有孔虫中玻璃质壳占绝对优势，比例为93 . 87 100 。 |
| 10. | Saw excitated by input idt is divided axisymmetrily ( y type ) or centrosymmetrily ( s type ) into two pathes and detected by their output idts . there is a mass loading area located accurately in each acoustic path and fabricated by photolithography technology in y type and s type mass loading sensor devices . as the characteristics of saw sensor are greatly influenced by temperature , these sensors have one acoustic path for reference another acoustic path for measurement in order to reduce the influence of temperature
它们各自具有一个输入idt和两个输出idt 。输入idt激发的saw经过耦合器按轴对称( y型)和中心对称( s型)分成两路，分别由输出idt检测输出。在y型和s型saw质量沉积效应传感器件的传播路径上都有一个由光刻工艺精确定位的质量沉积区。 |
