Rare earth elemental and Sr isotopic evidence for seawater intrusion event of the Songliao Basin 91 million years ago

Petrogenesis of lacustrine dolostone is closely related with paleo-lake water conditions.Here we report the high spatial-resolution petrographic and geochemical results of a lacustrine dolomite nodule from the Qingshankou Formation,the Songliao Basin.Sedimentary and elemental signatures confirm the protogenetic origin of this nodule and its effectiveness in recording geochemical characteristics of paleo-lake water during dolomitization.The low Y/Ho ratios,middle rare earth element(MREE)enrichment and subtle positive Eu anomalies within the nodule indicate a fresh water source.However,the Sr isotope values in the core of the nodule(0.7076-0.7080)are close to contemporaneous seawater(0.7074),yet different from the modern river(0.7120)and the host black shale(0.7100).On the premise of excluding the influence of hydrothermal fluids,the significantly low strontium isotope values of the lacustrine dolomite might be caused by seawater interference during dolomitization.Our findings demonstrate that lacustrine dolomite within black shales is not only a faithful tracer of diagenetic water environment,but also a novel and easily identified mineralogical evidence for episodic seawater intrusion event(91 Ma)in the Songliao Basin,which supplements other paleontological and geochemical evidence.

电脉冲处理对激光沉积Ti-6Al-4V合金强度各向异性的影响

为消除激光沉积Ti−6Al−4V合金的强度各向异性,利用拉伸试验、光学显微组织观察、扫描电子显微观察、电子背散射衍射分析和透射电子显微观察研究电脉冲对激光沉积Ti−6Al−4V合金显微组织与强度的影响。结果显示,随着施加电压从0增加到130 V,β柱状晶内的显微组织按如下顺序演化:α′马氏体→集束α组织→网篮α组织。130 V电脉冲处理会弱化β柱状晶内马氏体织构。沉积态Ti−6Al−4V合金表现出约6.2%的屈服强度各向异性;经130 V的电脉冲处理后,屈服强度各向异性减小到0.6%。这主要是由于沿不同方向变形时,130 V电脉冲处理样品表现出近似相同的施密特因子分布。