A Genetic Model for the Layered Intrusions and Related V—Ti—Magnetite Deposits in Panzhihua—Xichang Region,Southwest China

The area studied had developed into an inactive continental margin on the western edge of the Yangtze plate during the Jinning period in Proterozoic time.The Yangtze plate drifted from the south northwards in Paleozoic time and reached about 9oS between Late Cambrian and Early Ordovician .The alkalic olivine basalt magma,which was produced via 2-5% partial melting of a fractionated mantle and was accumulated in a deep-seated magma chamber near the Moho.found its way upward along the reviving boundary faults into the upper crust.Two types of layered intrusions,basic and ultrabasic-basic,crystallized from the magma at different pressures.The high initial oxygen fugacity of the magma provides a favorable condition for the deposition of Fe-Ti oxides in the early stage of magmaevolution,resulting in large-sized early magmatic deposits.Magma crystallization may have been interrupted and repeated as a result of pulsative magma influx,giving rise to rhythmic cycles (including the corresponding V-Ti-magnetite ore beds).The magma was stratified owing to double diffusion at the crystallization front and convection was thus occasioned by the density gradient.This has greatly complicated the sequence as would be expected from normal crystallization.     

单轴挤压应力作用下岩石中产生的裂隙的形状分布

根据P波速度数据可推测单轴应力状态下岩石样品中所产生裂隙的形状分布。施加于岩石样品的单轴压力达到一定应力范围,轴应力撤除后,测得样品中P波速作为静压力的函数。通过变换轴向应力的大小周期地反复进行上述过程。假设所产生的裂隙形状为球状,便可以速度数据反过来求得具不同纵横比的裂隙孔隙率的分布。对原始岩石样品来说,纵横比大的裂隙的孔隙率(厚裂隙)大于纵横比小的(薄裂隙)。当岩石样品受到较大的单轴挤压时,薄裂隙的孔隙率增加,厚裂隙的孔隙率减少。这种结果可能解释为:(1)大量剪切裂隙的出现;(2)由于轴向挤压应力的解除开口裂隙封闭;(3)未受力以前存在于原始岩石样品中的厚裂隙解体。     

框架—剪力墙型结构的非线性随机地震反应和可靠性分析

框架-剪力墙结构在地震载荷作用下的非线性特性及其描述以及非线性随机反应分析是很复杂的。本文对剪力墙建议了一个能反映其主要弯曲和剪切非线性特性的简化模型,据此模型提出了框架-剪力墙结构非线性随机地震反应分析的等效线性化方法和以变形极限状态概率表示的地震可靠性分析方法,该方法比较简便实用,可用于剪力墙和框架-剪力墙型结构体系的非线性随机地震反应分析和可靠性分析。     

中国大陆主要强震区（带）地震危险性的灰色预测

本文根据我国大地构造背景和强震震中分布特征,划分出主要强震区(带)。通过对各区地震时间分布不均匀性的分析,划分出各区的强震集发时段。分别以各区强震集发时段的起、止时间为基本数据,运用灰色理论的基本方法,建立灰色预测模型。给出各强震区(带)本次和下次集发时段的灰色预测结果。