Cenozoic thermal history reconstruction of the Dongpu Sag,Bohai Bay Basin: Insights from apatite fission‐track thermochronology

Knowledge of the thermal history of the onshore Dongpu Sag (DPS), Bohai Bay Basin is important for understanding its tectonic development within a broader regional context and for elucidating its poorly studied source‐rock maturation history. To unravel DPS time‐temperature development, apatite fission‐track data were acquired from eight sandstone samples in three deep wells. Thermal history modelling indicates continuous heating during the rifting stage (early Eocene to late Oligocene), followed by cooling attributed to tectonic uplift between ~27 and ~16 Ma, which resulted in the removal of ~1,400 to 1,800 m of section. Reheating occurred during the subsidence stage from middle Miocene until present. Unlike typical passive continental margin basins, the DPS experienced accelerated post‐rifting subsidence from ~5.8 Ma, which was especially marked since ~2.6 Ma. This phase was probably triggered by normal fault reactivation, in combination with a variation in the deep heat flow pattern.     

Pb同位素剖面化探法在甘肃玛曲地区大水金矿深部找矿中的应用

攻深找盲是大水金矿矿山勘查的主要任务。根据Pb同位素示踪的有关理论和隐伏矿预测的方法,以甘肃玛曲大水金矿区为例,利用Pb同位素剖面化探法在大水金矿典型剖面70、72勘探线采集Pb同位素样品78个,进行成矿截止深度预测。取本区域的成矿V2截止值在22.4～234.36之间,70、72勘探线在3450m标高左右V2值分别为49.11、64.83,预测70～72勘探线深部及以西成矿截止深度在3000～3100m之间,还有400～500m的勘查空间,找矿潜力大,是今后矿区勘查的重点地段。     

卫星精密定轨的三频观测量IF组合法

随着全球卫星导航系统的发展,GNSS卫星发播多频观测量已成必然趋势。然而,目前IGS分析中心依然使用双频观测量的策略进行轨道、钟差等产品的解算,并没有顾及额外频点观测量对定轨产品带来的效益。本文使用两个双频无电离层组合（IF）作为观测模型,研究第三频点观测量对轨道、钟差及测站位置精度的改善。在观测方程中将卫星端的相位偏差分成时变和时不变分量,通过对两个IF组合的观测方程进行参数重组,推导了与IGS钟差产品基准一致的满秩观测模型。基于超宽巷、宽巷和窄巷双差模糊度构建策略,给出了三频观测量的模糊度固定方法。首先以12颗GPS Block IIF卫星为例,在两种测站布局情况下进行L1/L2 IF双频定轨（S1）、L1/L5 IF双频定轨（S2）、L1/L2和L1/L5两个IF组合的三频定轨（S3）试验。结果表明S3方案最优,测站均匀、不均匀情况下轨道结果S3相较S1分别改善10%以内、10%左右,钟差的RMS略有改善,STD分别改善6.4%、10.0%,而S3相较S2的改善幅度更小,改善百分比基本在5%以内。随后进行了BDS单系统定轨,并使用激光检核轨道,表明三频定轨较B1/B3定轨结果改善显著,但是较B1/B2方案结果改善微弱,可能的原因是天线相位中心误差改正值不准确。     

青海省贵德扎仓寺地热成因机理及开发利用建议

本文通过卫星热遥感影像及航磁、重力异常的宏观性解译热异常空间分布特征,野外实地调查温泉的出露条件和水化学特征,分析研究青海省贵德扎仓寺温泉的热源通道、入渗通道,从而讨论其成因机理和开发利用前景。研究结果表明:扎仓寺温泉泉口温度为93.5℃,与当地气压有关;大气降水和热水沟上游沟谷水为补给源,近东西向张裂为入渗通道,中三叠统砂板岩与印支期花岗闪长岩(γδ₅²)接触变质带为径流通道(热储层),中三叠统砂板岩为盖层,北北西向热光断裂(F₁)为热源通道,属断裂-深循环地热类系统类型;径流通道(热储层)温度可达136.0℃,具备蒸汽发电示范背景条件,而F₁断裂带附近2000 m深度温度可达195.0℃,具备干热岩开发利用前景。     

Effects of humic acid and Tween-80 on behavior of decabromodiphenyl ether in soil columns

The effects of organic matter, humic acid and Tween-80 on decabromodiphenyl ether (BDE-209) behavior in soil columns were investigated. The BDE-209 transport was simulated in 4-cm-length soil columns whether organic matter was added or not. A high concentration of BDE-209 was washed out of the soil column in the presence of 500 mg L^?1 of Tween-80 for forming and suspending contaminated soil colloids in more than 4-cm-length ones (especially in 10-cm-length ones). While the humic acid was to facilitate BDE-209 adsorption onto soil particles (like soil colloids), Tween-80 was to enhance BDE-209 movement in porous media. The significant concentration averaged from 0.2 to 0.1 μg L^?1 in soil columns of length from 10 to 24 cm with Tween-80 addition by comparing the estimated marginal means (p < 0.05, SPSS). Contrasted with humic acid-binding BDE-209 in soil particles, Tween-80 could carry contaminant soil colloids into deeper layers and even affect the final effluents of 25-cm-length columns. It was visibly presented that the BDE-209 concentration in the effluents was mainly induced by Tween-80. Thus, BDE-209 was carried by soil colloids to transport and pollute longer and wider soil distance with the help of the effective promoters and stabilizers of Tween-80 and humic acid in soil matrix.     

试论鄂尔多斯盆地奥陶系成钾条件及找钾方向

鄂尔多斯盆地奥陶纪含盐建造且具含钾性是目前世界已知的唯一特例 ,因此 ,对其成盐成钾条件及找钾方向的研究具有重要的意义。鄂尔多斯盆地构造及地层研究表明 ,奥陶系具有成盐成钾的有利条件 ,也具有盐层的良好保存条件。古成盐环境和古盐湖卤水生物、物化条件以及钾石盐岩分析表明 ,下奥陶统马家沟组五段六亚段和四亚段 (O1m5-6、O1m5-4 )是利于钾盐沉积的 ,即是找钾的有利层段 ;古构造和古地理研究表明了成钾的有利地区是 :西北次凹 ,南部次凹 ,西南部次凹和北部次凹。     

滇西保山地区晚寒武世火山岩的发现及其构造意义

滇西保山地区上岩箐—白岩凹林场一带的晚寒武世火山岩虽不甚发育,但分布广泛。早期为拉斑玄武岩、碱性玄武岩,晚期为钙碱性玄武岩。岩石地球化学特征表明,早期火山岩形成于伸展环境,晚期火山岩为消减作用产物。保山地体构造背景在晚寒武世由伸展环境向挤压环境转换,并形成寒武系与奥陶系之间的不整合,为东冈瓦纳大陆北缘由被动大陆边缘向主动大陆边缘转换提供了岩石学证据。     

川东及其周缘地区下寒武统龙王庙组储集层特征与控制因素

根据薄片、阴极发光、扫描电镜、岩石物性等分析化验资料以及测井资料,对川东及其周缘地区下寒武统龙王庙组储集层特征与控制因素进行研究。结果表明:(1)龙王庙组储集层岩性主要为颗粒碳酸盐岩,其次是粉-细晶白云岩。(2)龙王庙组储集层储集空间主要为粒间(溶)孔、晶间(溶)孔、粒内溶孔,构造缝和溶蚀缝发育;储集层基质孔隙度值和渗透率值低,平均值分别为4.25％和6.25×10^-3μm²,储集层类型包括孔隙型和裂缝-溶孔型2种。(3)龙王庙组储集层的形成和分布可能受到沉积作用、成岩作用、埋藏过程等3种控制因素的共同影响:沉积作用提供了储集层发育的地质基础;成岩作用是影响储集层发育的关键因素;埋藏方式影响储集层的最终形成,是川东地区龙王庙组储集层质量差于川中及川东南地区的原因之一。(4)综合储集层的岩性、物性、厚度及分布范围,认为川东及其周缘地区龙王庙组储集层以局限台地内滩体最为有利,局限潮坪次之。     

http://www.sciencedirect.com/science/article/pii/S1674987112000667

The brackish-water bivalve Waagenopema Tokuyama,1959 is reported from the Lower Jurassic Badaowan Formation at four localities,along the southern margin and western margin of the Junggar Basin. Taphonomic features recorded in the field indicate that it occurs in autochthonous or parautochthonous assemblages.The autecology of Waagenopema therefore yields information on the palaeoenvironment of the area.The restriction of Waagenopema to marine and brackish-water settings suggests that the sea water once reached these areas during the Sinemurian.This paper discusses the palaeogeographic implications and suggests an ingression of the sea water from the west to the western and southern part of the Junggar Basin.Additionally,the two Waagenopema species collected from the Haojiagou section in the Junggar Basin are taxonomically documented.