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Origin of dolomite in the Middle Ordovician peritidal platform carbonates in the northern Ordos Basin, western China 被引量:5
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作者 Xiao-Liang Bai Shao-Nan Zhang +2 位作者 qing-yu huang Xiao-Qi Ding Si-Yang Zhang 《Petroleum Science》 SCIE CAS CSCD 2016年第3期434-449,共16页
The carbonates in the Middle Ordovician Ma_5~5submember of the Majiagou Formation in the northern Ordos Basin are partially to completely dolomitized.Two types of replacive dolomite are distinguished:(1) type 1dol... The carbonates in the Middle Ordovician Ma_5~5submember of the Majiagou Formation in the northern Ordos Basin are partially to completely dolomitized.Two types of replacive dolomite are distinguished:(1) type 1dolomite,which is primarily characterized by microcrystalline(〈30 urn),euhedral to subhedral dolomite crystals,and is generally laminated and associated with gypsumbearing microcrystalline dolomite,and(2) type 2 dolomite,which is composed primarily of finely crystalline(30-100 urn),regular crystal plane,euhedral to subhedral dolomite.The type 2 dolomite crystals are truncated by stylolites,indicating that the type 2 dolomite most likely predated or developed simultaneously with the formation of the stylolites.Stratigraphic,petrographic,and geochemical data indicate that the type 1 dolomite formed from near-surface,low-temperature,and slightly evaporated seawater and that the dolomitizing fluids may have been driven by density differences and elevation-related hydraulic head.The absence of massive depositional evaporites in the dolomitized intervals indicates that dolomitization was driven by the reflux of slightly evaporated seawater.The δ~(18)O values(-7.5 to-6.1 ‰) of type1 dolomite are slightly lower than those of seawaterderived dolomite,suggesting that the dolomite may be related to the recrystallization of dolomite at higher temperatures during burial.The type 2 dolomite has lowerδ~(18)O values(-8.5 to-6.7 ‰) and Sr~(2+) concentration and slightly higher Na~+,Fe~(2+),and Mn~(2+) concentrations and~(87)Sr/~(86)Sr ratios(0.709188-0.709485) than type 1 dolomite,suggesting that the type 2 dolomite precipitated from modified seawater and dolomitic fluids in pore water and that it developed at slightly higher temperatures as a result of shallow burial. 展开更多
关键词 Carbonate platform Dolomitization Dolomite Middle Ordovician Ma_5~5 submember Dolomitizing fluids
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Application of endovascular pure electrocoagulation in the management of coronary artery perforation during percutaneous coronary intervention 被引量:1
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作者 qing-yu huang Bang-Wei WU +4 位作者 Bo JIN Wei SHEN Mazin Eisa Xin-Ping LUO Jian LI 《Journal of Geriatric Cardiology》 SCIE CAS CSCD 2021年第3期240-244,共5页
Coronary artery perforation(CAP)during percutaneous coronary intervention(PCI)is a serious complication associated with significant morbidity and mortality.Its incidence in the general PCI population has been reported... Coronary artery perforation(CAP)during percutaneous coronary intervention(PCI)is a serious complication associated with significant morbidity and mortality.Its incidence in the general PCI population has been reported to range from 0.50%to 0.58%.Meanwhile,in chronic total occlusion(CTO)PCI procedure,the incidence increased to 1.4%−4.4%.[1]Currently,most of CAPs are distally located and related to guidewire,especially hydrophilic guidewire manipulations.[2]To avoid urgent or emergency cardiac surgery,some commonly used techniques include balloon inflations,covered stents,and coil embolization stand as representative options in the treatment of CAP.[3]Despite the availability of treatment approaches,there is still a lack of a standard consensus about the optimal management of this challenging complication.Endovascular pure electrocoagulation is a new approach that has been reported in the management of small vessel hemorrhage disease in cerebrovascular intervention,it can also provide promising results in CAP management. 展开更多
关键词 CORONARY BALLOON treatment
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