北冰洋独特的变质沉积岩碎屑:是Alph海岭的原地产物还是来自2.6Ma之前的浮冰搬运?

从冰雪岛屿T-3采集的F1-380岩心位于Alpha海岭东部边缘的斜坡上,其为一长900km、宽500km的不规则宽广破碎背斜,被认为是构造演化仍然是个谜的地球上少数大规模地质构造之一.该段Alpha海岭的岩心包括M至A2岩性单元(全新世至上新世或中新世?),但岩心最下部含有千枚糜棱岩碎屑.     

Distribution and U-Pb Ages of Newly Recognized Regional-Scale Dyke Swarms of the Leo Man Craton

正Over 20 sets of dolerite dykes crosscutting Paleoproterozoic basement in West Africa were distinguished via the interpretation of regional and high resolution magnetic airborne data of West African Craton     

Effect of Faulting on Ordovician Carbonate Buried-Hill Reservoir Beds in Hetianhe Gas Field,Tarim Basin

Ordovician carbonate buried-hill reservoir beds in the Hetianhe (和田河) gas field,located in the Mazhatage (玛扎塔格) structural belt on the southern margin of the Bachu (巴楚) faulted uplift,southwestern Tarim basin,were studied.Based on field survey,core and slice observation,the general characteristics of carbonate buried-hill reservoir beds and specifically Ordovician carbonate buried-hill reservoir beds in the Hetianhe gas field were discussed.The karst zone of the reservoir beds in Hetianhe gas field was divided into superficial karst zone,vertical infiltration karst zone,lower subsurface flow karst zone,and deep sluggish flow zone from top to bottom.The effects of faulting on Ordovician carbonate buried-hill reservoir beds in the Hetianhe gas field were obvious.The faulting intensified the karstification and increased the depth of denudation.Faulting and subsequent fracture growth modified the reservoir beds and improved the physical property and quality of the reservoir beds.Moreover,faulting enhanced the development of the dissolution holes and fractures and increased the thickness of the effective reservoir beds.Meanwhile,faulting made the high porosity-permeability carbonate belts,which created conditions for the hydrocarbon accumulation,develop near the fault zone.     

Contribution of dust produced by binary merger ejecta

By means of a population synthesis code and by constructing a simple toy model of dust produced by asymptotic giant branch(AGB) stars, common envelope(CE) ejecta and binary merger ejecta, we estimate the dust product rates(DPRs) of these processes in the Milky Way. The total DPR from AGB stars is～ 6.7 × 10-4M yr-1, in which about 73% of dust grains are carbon, 24% are silicates and 3% are iron. The total DPR from CE ejecta is ～ 4.2 × 10-4M yr-1, in which about 83% of dust grains are silicates, about 12% are carbon and 5% are iron.The DPR from binary merger ejecta is less than 1/3 that from AGB stars or CE ejecta,and it could even be negligible under certain circumstances. Therefore, compared with AGB stars and CE ejecta, the contribution of dust produced by binary merger ejecta to total dust grains in the Milky Way is smaller or can be negligible.     

一九三五年春季飞机测候中之尘暴研究

近年以来政府增加飞机测候所,每日探测高空情形,尤注意于一九二五年春季发生于平原各省而致灾害之麈暴(Duststorm)。有时麈沙非常浓厚,飞行只能停止,但大多数仍可飞行,而沙麈之高度亦经测定。在最强烈之麈暴中,曾测得其高度,约达一万四千英尺,在其他数次之实例,其上部之界限皆不及一万八千英尺。在 O(?)lahomo     

全新世时期热带太平洋西部表层温度和盐度的降低

在现今的气候条件下,热带太平洋西部(WTP)的表层水盐度偏低,向该盆地的东部有增加的趋势。热带太平洋表层水的盐度被认为受大气层对流、降雨、蒸发和大洋动力等综合因素的控制,而年间时间表上的明显变化多与厄尔尼诺-南方涛动(ENSO)循环有关,然而,人们很少知道这个大洋-大气耦合系统在百年、千年时间表上的变化情况。     

利用黄土中的碳同位素半定量地重建古温度

在相对稳定的气候阶段,土壤中的CO2与其中的碳酸盐之间处于同位素平衡状态,这意味着二者的碳同位素分馏值可作为地质温度计估算古温度。对中国洛川黄土剖面的10组黄土-古土壤序列L1-1-S8同时做了碳酸盐和有机质的碳同位素分析。由于这些地层单元可以与深海氧同位素记录的2-21阶段对比,其中L1-1-L2可与南极Vostok冰心的大气CO2浓度记录对比,由此通过相关分析确定了各地层形成时的平均大气CO2浓度及其δ^183C值,再根据Cerling模型,用有机质δ^13C值代替土壤呼吸CO2的δ^13C,算出土壤CO2的δ^13值。将该值与次生碳酸盐的δ^13C值代入Deines分馏方程可算出各地层单元的古温度。该温度代表了平均深度约30cm处的土壤温度,相当于当时的夏季大气温度。所有数据与黄土-古土壤地层学记录的气候变化吻合,定量地反映了近800ka来黄土高原古气候的变化。     

Artisanal ceramic factories using wood combustion:A nanoparticles and human health study

The ceramics industry,resulting from developments of modern compounds,is a segment of great influence in worldwide sustainability.Artisanal ceramic factories based on wood combustion have significant risks for the creation and discharge of atmosphere nanoparticles(NPs)and ultra-fine particles(UFPs).At present,there is insufficient recognition on the influence of engineered-NPs on the atmosphere and health.Real improvements are indispensable to diminish contact with NPs.The present study demonstrates the main NPs and UFPS present in an area of intense artisanal wood-combustion ceramic manufacturing.Particulate matter was sampled for morphological,chemical,and geochemical studies by sophisticated electron microbeam microscopy,X-Ray Diffraction,and Raman spectroscopy.From NPs configuration(<10 nm)we identify nucleation.Several amorphous NPs(>10 nm)were produced around the studied artisanal ceramic factories.This study presents an indication of the recent information on population and work-related contact to NPs in the artisanal ceramic factories and their influence on health.     

Geochemical Characteristics and Tectonic Environment of Quartz Porphyry in Northwestern Guangxi

Please?refer?to?the?attachment(s)?for?more?details.     

Porphyry-style Mineral Deposit Taxonomy—Lessons from the USGS Global Assessment

Please refer to the attachment(s) for more details