Noble gases in corundum megacrysts from the basalts in Changle, Shandong Province, eastern China

This study presents noble gaseous data of the corundum megacrysts from the Cenozoic basalts in Changle, Shandong Province, eastern China. It is known that no noble gaseous data of corundum megacryst have been documented before. The 3He/4He ratios (1.13-7.37 Ra) of the corundums from Changle vary from atmosphere to MORB values; the 20Ne/22Ne (9.67-10.75) and 21Ne/22Ne (0.0280-0.0372) data define two linear trends on Ne three-isotope diagram, respectively, along the MFL and the correlation line between atmosphere and MORB; the 38Ar/36Ar (0.177-0.194) ratios, the 40Ar/36Ar (280.9 -404.2) ratios and the 128-136Xe/132Xe ration with obvious 129Xe excess are generally higher than at-mospheric component, but the 40Ar/36Ar ratios are much closer to atomospheric ratio. The isotopic compositions of noble gases (particularly for He and Ar) of the corundums are similar to those of py-roxene, anorthoclase megacrysts, and mantle-derived xenoliths from this area, and those of man-tle-derived xenoliths from several areas in eastern China. Therefore, the noble gases trapped in the corundums probably are from mantle source, representing a ‘mixed fluid' produced by the interaction between the lithospheric mantle and fluids releasing from the convective plate. Both the noble gas isotopic compositions and the oxygen isotopic compositions of the solid corundums are not the characteristics of crustal source. These suggest that the corundums crystallized from mantle-derived magmas with minimal crustal contamination.     

From deep basin gas to diagenetic trap—An example from the Yulin Gas Field in the Ordos Basin

In the updip portion of the Yulin Gas Field in the Ordos Basin, there are no any structural, stratigraphic and sedimentary lithologic seals. Using thin-section petrography, ultraviolet fluorescence microscopy, micro-thermometry and Raman microspectrometry, this paper finds out the diagenetic trap and studies the diagenetic history of this field. It was revealed that three phases of diagenesis and hydrocarbon charging happened in late Triassic, late Jurassic and the end of early Cretaceous respectively. In the first two phases, acid geofluid entered the reservoir and caused dissolution and cementation. Although the porosities had been increased, further compaction accompanying re-subsidence resulted in tight sandstone and conglomerates. Till the end of the early Cretaceous, bulk of gas migrated into the tight reservoir. Cementation, however, kept on in the updip portion of this field due to low gas saturation and formed the diagenetic trap. The mechanism for gas accumulation was changed from deep basin gas to diagenetic trap, which offers a sealing condition that can retain gas for much longer time.     

高矿化度水压裂液螯合剂的研制

用油田产出水、返排水等高矿化度水作为配液水配制压裂液时,由于其中多种高价、变价金属离子含量较高,易与羟丙基瓜胶上的羟基发生配位竞争,在高分子表面容易形成聚团,严重影响了瓜胶的溶胀和交联性能。为此,研制开发出一种螯合剂,可解决瓜胶溶胀难、黏度低等问题。对该体系性能评价实验结果表明,用加入该螯合剂的高矿化度水配制羟丙基瓜胶压裂液,加入交联剂后可在3~4 min交联,且交联冻胶弹性好。在90℃,170 s~(-1)下连续剪切1.5 h,黏度为101.32 m Pa·s,使配制的压裂液对金属离子具有良好的耐受性和螯合性,可形成有效稳定的交联冻胶,并有效改善其耐温耐剪切性能。     

Google Earth平台在虚拟旅游上的应用

随着Google Earth技术含量的不断提高,基于Google Earth的应用技术在国内外已成为研究的热点。该文章提出利用Google Earth搭建动态的虚拟旅游平台,实现三维化的人、景交互界面。该方法利用Google Earth识别KML文件的技术,使用KML文件加载地标的信息、图片、视屏,使用者通过点击景点的地标,连接到Google Earth就可以全方位的浏览地标所在景点的信息。使用Google Earth能够全方位观察场景,整体感强,具有交互性和沉浸感,用户能产生＂虚拟游历＂的感觉。