Structural Analysis of the Luowei Orefield in Xidamingshan,Guangxi, China     

Saisai Li  Zuohai Feng  Wei Fu  Zemin Li  Rongguo Hu 《Resource Geology》2020,70(1):89-107

Many types of hydrothermal deposits (e.g. W, Bi, Pb, Zn, Ag) are confined by faults and hidden granodiorite in the Luowei Orefield in Xidamingshan, Guangxi, China. The orebodies in the Luowei W–Bi deposit are predominantly layered and distributed along bedding in sandstones of the Cambrian Xiaoneichong Formation. The orebodies in the Lujing Pb–Zn deposit are controlled mainly by west‐south‐west (WSW)‐trending faults, and those in the Fenghuangshan Ag deposit are controlled mainly by west‐north‐west (WNW)‐trending faults, which were reverse faults during mineralization and were later reactivated as sinistral strike‐slip faults. The Luowei fault was formed postmineralization and resulted in sinistral displacement of the subsurface granodiorite and the Cambrian strata. A tectonomagmatic mineralization model of the Luowei Orefield is proposed, and the following conclusions were made. (i) Under a regional N–S compressive stress regime, WSW‐ and WNW‐trending reverse faults and N–S‐trending tensional fractures were formed. (ii) Magma intruded along the tensional fractures. Under the force of magmatic thermodynamics, mineralizing fluid migrated along bedding planes in sandstones and formed W–Bi orebodies at favorable sites. Some fluid migrated along WSW‐ and WNW‐trending faults to sites farther from the magma source, forming vein‐type Pb–Zn and Ag orebodies. (iii) After mineralization, under ~E–W compression, a NW‐trending left‐lateral slip fault was formed, cutting the subsurface granodiorite and orebodies. Concurrently, sinistral shear slip occurred on WNW‐trending ore‐controlling faults. However, the small displacement on these faults did not change the overall distributions of the rock mass and orebodies.  相似文献   

True Type格式"地质矿产符号库"特点介绍   总被引：1，自引：0，他引：1  

刘冶兵  王立民  陈雷  徐卫 《吉林地质》2004,23(2):69-71

“地质矿产符号库”是一套采用国际先进技术、符合国内行业标准的专业字库。具有4大特点,可用8个字概括：“美观、统一、规范、通用”。  相似文献   

Using trace elements of magnetite to constrain the origin of the Pingchuan hydrothermal low-Ti magnetite deposit in the Panxi area,SW China     

Yanjun Wang  Weiguang Zhu  Hong Zhong  Zhongjie Bai  Junhua Yao  Chong Xu 《Acta Geochimica》2019,(3):376-390

The Pingchuan iron deposit, located in the Yanyuan region of Sichuan Province, SW China, has an ore reserve of 40 Mt with ~60 wt% Fe. Its genesis is still poorly understood. The Pingchuan iron deposit has a paragenetic sequence of an early Fe-oxide–Pyrite stage(Ⅰ) and a late Fe-oxide–pyrrhotite stage(Ⅱ). Stage Ⅰ magnetite grains are generally fragmented, euhedral–subhedral, largesized crystals accompanying with slightly postdated pyrite.Stage Ⅱ magnetite grains are mostly unfragmented, anhedral, relatively small-sized grains that co-exist with pyrrhotite. Combined with micro-textural features and previously-obtained geochronological data, we consider that these two stages of iron mineralization in the Pingchuan deposit correspond to the Permian ELIP magmatism and Cenozoic fault activity event. Both the Stage Ⅰ and Ⅱ magnetites are characterized with overall lower contents of trace elements(including Cr, Ti, V, and Ni) than the ELIP magmatic magnetite, which suggests a hydrothermal origin for them. ‘‘Skarn-like' enrichment in Sn, Mn, and Zn in the Stage Ⅰ magnetite grains indicate significant material contributions from carbonate wall-rocks due to water–rock interaction in ore-forming processes. Stage Ⅱ magnetite grains contain higher Mn concentrations than Stage Ⅰ magnetite grains, which possibly implies more contribution from carbonate rocks. In multiple-element diagrams, the Stage Ⅰ magnetite shows systematic similarities to Kiruna-type magnetite rather than those from other types of deposits. Combined with geological features and previous studies on oxygen isotopes, we conclude that hydrothermal fluids have played a key role in the generation of the Pingchuan low-Ti iron deposit.  相似文献   

Lipid biomarker composition in surface sediments from the Carlsberg Ridge near the Tianxiu Hydrothermal Field     

Shengyi Mao  Hongxiang Guan  Lihua Liu  Xiqiu Han  Xueping Chen  Juan Yu  Yongge Sun  Yejian Wang 《海洋学报(英文版)》2021,40(8):53-64

Hydrothermal venting has a profound effect on the chemical and biological properties of local and distal seawater and sediments. In this study, lipid biomarkers were analyzed to examine the potential influence of hydrothermal activity on the fate of organic matter(OM) in surface sediments around Tianxiu Hydrothermal Field in the Carlsberg Ridge(CR), Northwest Indian Ocean. By comparing the biomarker distributions of the samples with that of other typical hydrothermal sediments in the mid ocean ridge, it is shown that the location of the samples is not affected by the hydrothermal activity. The relatively low abundances of terrestrial n-alkyl lipids and riverine1,15-C32 diol suggested a minor contribution of terrigenous OM to the study area. The bacteria contributed predominantly to sedimentary marine OM; however, other marine source organisms, e.g., eukaryotes(i.e.,phytoplankton and fungi) could not be completely neglected. The marine-originated biomarkers showed significantly variable distributions between the two sediments, suggesting different dynamic physical and biogeochemical processes controlling the fate of marine OM. This study identified various diagnostic biomarkers(5,5-diethyl alkanes, diols and β-OH FAs), which may have significant environmental implications for future works in this region.  相似文献   

三疣梭子蟹(Portunus trituberculatus)I 型Crustin抗菌肽的基因克隆与真核重组表达   总被引：1，自引：0，他引：1       下载免费PDF全文

申望  叶茂  石戈  王日昕 《海洋与湖沼》2010,41(3):371-377

Crustin 是目前报道广泛存在于甲壳类中的一类具有广谱抗菌活性的抗菌肽, 主要由甲壳类血淋巴细胞合成。本研究采用RACE 技术和真核表达技术, 进行了三疣梭子蟹Crustin 基因的克隆和重组表达研究。结果表明, 在三疣梭子蟹血细胞Crustin 基因cDNA 全序列中, 开放阅读框编码110个氨基酸残基的Crustin 前体, Crustin 前体由N 端21 个氨基酸残基的信号肽、富含Cys 结构域和C端WAP 结构域三部分组成, 属于I 型Crustin, 构建的分泌型真核表达质粒pVT102U/α-crustin 转化酿酒酵母S78, 经RT-PCR 和SDS-PAGE 电泳验证, 表明重组Crustin 表达成功。  相似文献