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101.
ZHANG Xiaopei HAN Runsheng ZHAO Dong QIU Wenlong HE Jiaojiao CUI Junhao 《《地质学报》英文版》2017,91(Z1):249-250
<正>1 Introduction The super-large Huize lead-zinc ore district is one of the most representative lead-zinc deposits in Northeastern Yunnan poly-metallic deposit concentration district.So far,studies(Liu and Lin,1999;Han et al.,2007)on the type of deposits like the Huize lead-zinc deposit,focused on deposit genesis,the sources of metallogenic materials, 相似文献
102.
Permian High Ba-Sr Granitoids: Geochemistry, Age and Tectonic Implications of Erlangshan Pluton, Urad Zhongqi, Inner Mongolia 总被引:1,自引:0,他引:1
Abstract: Erlangshan Pluton from Urad Zhongqi, central Inner Mongolia, is located in the middle segment of the northern margin of the North China Plate. The rocks consist mainly of diorites with gneissic structure. Petrochemical characteristics reveal that the diorites belong to metaluminous, high-potassium calc-alkaline series, with chemical signatures of I-type granites. They are characterized by low SiO2 contents (56.63%–58.53%) and A/CNK (0.90–0.96), high Al2O3 contents (17.30%–17.96%) and Na2O/K2O ratios (1.20–1.70), enrichment in large ion lithophile elements (LILE, e.g., Ba=556–915 ppm, Sr=463–595 ppm), and relative depletion in high field strength elements (HFSE, e.g., Nb, Ta, Ti) in primitive mantle-normalized spidergram, and right-declined rare earth element patterns with slightly negative Eu anomalies (d?Eu=0.72–0.90). They have Sr/Y ratios (20–25) evidently less than Kebu Pluton (49–75) to its east. Sensitive high resolution ion micro-probe U-Pb zircon dating of the diorites has yielded an intrusive age of 270±8?Ma. This leads us to conclude that Erlangshan diorites were formed by mixing between the middle or lower crustal-derived magma and minor mantle-derived mafic magma, followed by fractional crystallization, which was trigged by crustal extension and fault activity in post-collisional setting. 相似文献
103.
Relationship Between the Western Pacific Subtropical High and the Subtropical East Asian Diabatic Heating During South China Heavy Rains in June 2005
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Based on the daily NCEP/NCAR reanalysis data, the position variation of the western Pacific subtropical high (WPSH) in June
2005 and its relation to the diabatic heating in the subtropical East Asia are analyzed using the complete vertical vorticity
equation. The results show that the position variation of the WPSH is indeed associated with the diabatic heating in the subtropical
East Asian areas. In comparison with June climatology, stronger heating on the north side of the WPSH and relatively weak
ITCZ (intertropical convergence zone) convection on the south side of the WPSH occurred in June 2005. Along with the northward
movement of the WPSH, the convective latent heating extended northward from the south side of the WPSH. The heating to the
west of the WPSH was generally greater than that inside the WPSH, and each significant enhancement of the heating field corresponded
to a subsequent westward extension of the WPSH. In the mid troposphere, the vertical variation of heating on the north of
the WPSH was greater than the climatology, which is unfavorable for the northward movement of the WPSH. On the other hand,
the vertical variation of heating south of the WPSH was largely smaller than the climatology, which is favorable for the anomalous
increase of anticyclonic vorticity, leading to the southward retreat of the WPSH. Before the westward extension of the WPSH
in late June 2005, the vertical variation of heating rates to (in) the west (east) of the WPSH was largely higher (lower)
than the climatology, which is in favor of the increase of anticyclonic (cyclonic) vorticity to (in) the west (east) of the
WPSH, inducing the subsequent westward extension of the WPSH. Similar features appeared in the lower troposphere. In a word,
the heating on the north-south, east-west of the WPSH worked together, resulting in the WPSH extending more southward and
westward in June 2005, which is favorable to the maintenance of the rainbelt in South China. 相似文献
104.
Gravity Flow on Slope and Abyssal Systems in the Qiongdongnan Basin, Northern South China Sea 总被引:3,自引:0,他引:3
SU Ming XIE Xinong LI Junliang JIANG Tao ZHANG Cheng HE Yunlong TIAN Shanshan ZHANG Cuimei 《《地质学报》英文版》2011,85(1):243-253
The study of new seismic data permits the identification of sediment gravity flows in terms of internal architecture and the distribution on shelf and abyssal setting in the Qiongdongnan Basin (QDNB). Six gravity flow types are recognized: (1) turbidite channels with a truncational basal and concordant overburden relationship along the shelf edge and slope, comprising laterally-shifting and vertically-aggrading channel complexes; (2) slides with a spoon-shaped morphology slip steps on the shelf-break and generated from the deformation of poorly-consolidated and high water content sediments; (3) slumps are limited on the shelf slope, triggered either by an anomalous slope gradient or by fault activity; (4) turbidite sheet complexes (TSC) were ascribed to the basin-floor fan and slope fan origin, occasionally feeding the deep marine deposits by turbidity currents; (5) sediment waves occurring in the lower slope-basin floor, and covering an area of approximately 400?km2, were generated beneath currents flowing across the sea bed; and (6) the central canyon in the deep water area represents an exceptive type of gravity flow composed of an association of debris flow, turbidite channels, and TSC. It presents planar multisegment and vertical multiphase characteristics. Turbidite associated with good petrophysical property in the canyon could be treated as a potential exploration target in the QDNB. 相似文献
105.
Pyrite framboids were found in the Permian-Triassic boundary at Meishan Section, while their sulfur isotopes were determined. The majority of framboids is less than 5 μm in diameter, with some large-sized framboids. Also, euhedral gypsums were observed in the boundary clay. The authors suppose that most of the pyrite framboids formed just below the redox boundary and stopped growing after entering the lower water column. The result indicates that it was probably lower dysoxia condition in the temporal ocean. Moreover, the authors also presume that some pyrite was oxidated to sulfates accompanying the fluctuation of redox condition, which would probably be the origin of the negative sulfur isotopes of gypsum and CAS reported before. In addition, sulfur isotope of framboidal pyrite suggests that sulfur is originated from bacterial sulfate reduction in anoxic condition. Therefore, this study confirms that the ocean was widely anoxic during the Permian-Triassic transitional period. However, the redox condition in temporal ocean was probably not stable, with short-term fluctuations. 相似文献
106.
Heat flow pattern, base of methane hydrates stability zones and BSRs in Shenhu Area, northern South China Sea 总被引:2,自引:2,他引:0
ZHANG Yi HE Lijuan WANG Jiyang XU Xing SHA Zhibing GONG Yuehu WANG Hongbing LIANG Jinqiang 《海洋学报(英文版)》2011,30(1):59-67
Using the collected 433 heat flow values, we estimated the bases of methane hydrate stability zone (BHSZ), in northern South China Sea (NSCS). Through comparing BHSZs with the depths of bottom simulating reflectors (BSRs), in Shenhu Area (SA), we found that there are big differences between them. In the north of SA, where the water depth is shallow, many slumps developed and the sedimentation rate is high, it appears great negative difference (as large as -192%). However, to the southeast of SA, where the water depth is deeper, sedimentation rate is relatively low and uplift basement topography exists, it changes to positive difference (as large as +45%). The differences change so great, which haven’t been observed in other places of the world. After considering the errors from the process of heat flow measurement, the BSR depth, the relationship of thermal conductivity with the sediments depth, and the fluid flow activities, we conclude that the difference should be not caused by these errors. Such big disagreement may be due to the misunderstanding of BSR. The deviant “BSRs” could represent the paleo-BSRs or just gas-bearing sediment layers, such as unconformities or the specific strata where have different permeability, which are not hydraterelated BSRs. 相似文献
107.
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110.
HE Tianrong LI Ting Yang Ruidong LUO Guangjun LANG Xiaofang An Yanling YAN Haiyu 《中国地球化学学报》2013,32(1):104-109
In this paper, the relationship between sulfate reduction potential and mercury methylation potential was studied in the Aha, Baihua and Hongfeng reservoirs from Guiyang City. The methylmercury (MeHg) concentrations of lake water in the Aha Reservoir were greatly elevated as compared to those of the Hongfeng and Baihua reservoirs, which was correlated with its distinctly high SRB abundance, SO42-, and S2- concentrations. Among the three reservoirs, however, the highest MeHg was observed in in the top several centimenters of pore water profile in the Hongfeng Reservoir where the lowest S2- in pore water occurred. The distributions of MeHg in lake water and pore water showed the highest methylation potential occurred at water-sediment surface for the Aha Reservoir and the in the top several centimenters of sediments for the Hongfeng Reservoir. It is guessed that the highest mercury methylation only occurs at the sites with certain sulfide concentrations. 相似文献