复杂断裂带宽、窄方位角勘探技术评价与研究

通过对中国西部吐鲁番盆地北部山前带的宽、窄方位角地震数据进行对比分析研究表明:不同窄方位观测时,由于观测方向与断裂走向斜交存在较为严重的构造假象,并造成小断层难以成像.对于断裂带而言,不同方向窄方位角观测成像阴影带不同.全(宽)方位角观测可以获得各个方向小断层比较好的成像,同时也可以有效地获得断裂带的空间范围.在此基础上,通过随观测方位角不同的地震属性的变化来寻找和研究裂缝性储层发育区和估计裂缝发育的主要方向.     

The final rifting evolution in the South China Sea

Seismic reflection data imaging conjugate crustal sections at the South China Sea margins result in a conceptual model for rift-evolution at conjugate magma-poor margins in time and space.The wide Early Cenozoic South China Sea rift preserves the initial rift architecture at the distal margins. Most distinct are regular undulations in the crust–mantle boundary. Individual rift basins are bounded to crustal blocks by listric normal faults on either side. Moho uplifts are distinct beneath major rift basins, while the Moho is downbended beneath crustal blocks, with a wavelength of undulations in the crust–mantle boundary that approximately equals the thickness of the continental crust. Most of the basin-bounding faults sole out within the middle crust. At the distal margins, detachment faults are located at a mid-crustal level where a weak zone decouples crust and mantle lithosphere during rifting. The lower crust in contrast is interpreted as being strong. Only in the region within about 50 km from the Continent–Ocean Transition (COT) we suggest that normal faults reach the mantle, enabling potentially a coupling between the crust and the mantle. Here, at the proximal margins detachment fault dip either seaward or landward. This may indicate the presence of exhumed mantle bordering the continental margins.Post-rift shallow-water platform carbonates indicate a delay in subsidence during rifting in the South China Sea. We propose that this is an inherent process in highly extended continental margins and a common origin may be the influx of warm asthenospheric material into initially cool sub-lithospheric mantle.On a crustal-scale largely symmetric process predominate in the initial rifting stage. At the future COT either of the rift basin-bounding faults subsequently penetrates the entire crust, resulting in asymmetry at this location. However, asymmetric deformation which is controlled by large scale detachment faulting is confined to narrow areas and does not result in a margin-wide simple-shear model. Rather considerable along-margin variations are suggested resulting in alternating “upper and lower plate” margins.     

资源三号卫星传感器校正产品的精度评估

分别选取资源三号(ZY-3)卫星平地和山地区域的前后视影像,量测20个GPS点作为控制点和检查点,对卫星传感器校正产品定位精度进行验证。通过区域网平差算法对传感器校正产品(SC)自带的有理函数模型(RPC)进行优化,消除系统误差。实验结果表明:在地形平坦地区ZY-3卫星SC产品的平面定位精度可达3.275 m,高程定位精度可达1.686 m;在地形起伏较大的山区平面定位精度可达4.335 m,高程定位精度可达3.628 m,满足1∶50 000地形图测绘的要求。     

电磁测深方法研究

为能够实施电磁测深新方法的基本原理,并为研制探测仪器提供一些依据,分析和讨论了源信号为尖脉冲时,入射波与地层反射波通过二阶带通滤波器的输出波形;利用反射波与入射波前沿瞬态叠加的波形,反演地层的电导率和厚度的方法及与探测仪器有关的主要问题等内容. 结果表明,反演仍能给出惟一解,并具有可实践性.     

菲律宾蛤仔(Ruditapes philippinarum)大连群体家系建立及生长比较

于2008年6月,以大连野生型蛤仔为材料,采用巢式设计即1个雄性亲本与3个雌性亲本交配的方式建立了菲律宾蛤仔15个半同胞家系(A,B,…,O)和45个全同胞家系(A1,A2,A3,…,O1,O2,O3)。对各家系的壳长、壳宽、壳高、鲜重等各项指标进行了方差分析和多重比较。结果表明,3、4、5月龄,菲律宾蛤仔45个全同胞家系的表型性状具有显著差异,且各月龄的差异趋势基本一致。5月龄时,从其生长性状上看,家系F2、G2、G3表现出明显的生长优势,壳长分别提高28.43%、24.72%、30.53%,壳宽分别提高21.14%、22.3%、25.58%,壳高分别提高30.88%、26.96%、25.25%,鲜重分别提高50.00%、68.42%、44.12%。从其存活上看,家系E3的四个表型性状在全同胞家系中最小,但存活数量最多为2269粒,表现出很强的抗逆性;具有生长优势的家系F2存活个数最少仅为43粒,抗逆性相对最差。从其产量上看,家系N3、I1、E3、C1、N1、G2产量较高,分别比平均产量提高了77.8%、75.61%、75%、69.45%、53.96%、50.19%。综合以上各项指标家系G2、G3、N3、E3、I1、C1、N1可作为优良的家系育种材料,在下一步育种工作中可以利用家系选择及家系杂交的方法对7个家系进行遗传改良。