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为研究敦煌盆地侏罗纪原型盆地性质及沉积环境演化,本文利用地震资料、航磁资料、野外地质考察资料、同位素定量测年数据,基于前人在阿尔金断裂系构造理论成果,对敦煌盆地基底岩性组成、深部动力学背景、盆地发育时限和盆地性质做了系统研究,认为敦煌盆地与塔里木盆地、柴达木盆地、酒泉盆地的前侏罗纪基底组成不相同,是一个相对独立的盆地。敦煌地块的南部边界为红柳沟—拉配泉断裂,西部边界为民丰—且末断裂带,阿尔金主断裂为敦煌盆地的东部边界。三危山断裂是分割敦煌盆地南北凹陷的控凹断裂,民丰—且末断裂、红柳沟—拉配泉断裂、阿尔金主断裂是控盆断裂。青藏高原南缘的北向超深俯冲、北缘陆内南向的浅俯冲、深部地幔羽结构等多元驱动机制导致敦煌地块显生宙以来大部分时间处于隆升剥蚀状态,很少接受沉积,至侏罗纪塌陷形成敦煌湖盆。敦煌盆地在三叠纪和晚侏罗世—早白垩世青藏高原两次重大的碰撞造山之间的松弛拉张期形成了侏罗纪沉积盆地。敦煌盆地发育经历3个阶段：早侏罗世填平补齐阶段,中侏罗世断陷阶段和晚侏罗世坳陷阶段,其中中侏罗世断陷阶段为主成盆期。 相似文献
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Abdur Rashid Muhammad Ayub Asif Javed Sardar Khan Xubo Gao Chengcheng Li Zahid Ullah Tariq Sardar Juma Muhammad Shahla Nazneen 《地学前缘(英文版)》2021,12(3):101128
This study investigates the values of pH, total dissolved solids (TDS), elevation, oxidative reduction potential (ORP), temperature, and depth, while the concentrations of Br, and potentially harmful metals (PHMs) such as Cr, Ni, Cd, Mn, Cu, Pb, Co, Zn, and Fe in the groundwater samples. Moreover, geographic information system (GIS), XLSTAT, and IBM SPSS Statistics 20 software were used for spatial distribution modeling, principal component analysis (PCA), cluster analysis (CA), and Quantile-Quantile (Q-Q) plotting to determine groundwater pollution sources, similarity index, and normal distribution reference line for the selected parameters. The mean values of pH, TDS, elevation, ORP, temperature, depth, and Br were 7.2, 322 mg/L, 364 m, 188 mV, 29.6 °C, 70 m, 0.20 mg/L, and PHMs like Cr, Ni, Cd, Mn, Cu, Pb, Co, Zn, and Fe were 0.38, 0.26, 0.08, 0.27, 0.36, 0.22, 0.04, 0.43 and 0.86 mg/L, respectively. PHMs including Cr (89%), Cd (43%), Mn (23%), Pb (79%), Co (20%), and Fe (91%) exceeded the guideline values set by the world health organization (WHO). The significant R2 values of PCA for selected parameters were also determined (0.62, 0.67, 0.78, 0.73, 0.60, 0.87, ?0.50, 0.69, 0.70, 0.74, ?0.50, 0.70, 0.67, 0.79, 0.59, and ?0.55, respectively). PCA revealed three geochemical processes such as geogenic, anthropogenic, and reducing conditions. The mineral phases of Cd(OH)2, Fe(OH)3, FeOOH, Mn3O4, Fe2O3, MnOOH, Pb(OH)2, Mn(OH)2, MnO2, and Zn(OH)2 (?3.7, 3.75, 9.7, ?5.8, 8.9, ?3.6, 2.2, ?4.6, ?7.7, ?0.9, and 0.003, respectively) showed super-saturation and under-saturation conditions. Health risk assessment (HRA) values for PHMs were also calculated and the values of hazard quotient (HQ), and hazard indices (HI) for the entire study area were increased in the following order: Cd>Ni>Cu>Pb>Mn>Zn>Cr. Relatively higher HQ and HI values of Ni, Cd, Pb, and Cu were greater than one showing unsuitability of groundwater for domestic, agriculture, and drinking purposes. The long-term ingestion of groundwater could also cause severe health concerns such as kidney, brain dysfunction, liver, stomach problems, and even cancer. 相似文献
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The symmetrical body of flatfish larvae changes dramatically into an asymmetrical form after metamorphosis. The molecular mechanisms responsible for this change are poorly understood. As an initial step to clarify these mechanisms, we used representational difference analysis of cDNA for the identification of genes active during metamorphosis in the Japanese flounder, Paralichthys olicaceus. One of the up-regulated genes was identified as creatine kinase muscle type 1 (CK-M1). Sequence analysis of CK-M1 revealed that it spanned 1 708 bp and encoded a protein of 382 amino acids. The overall amino acid sequence of the CK-M1 was highly conserved with those of other organisms. CK-M1 was expressed in adult fish tissues, including skeletal muscle, intestine and gill. Whole mount in-situ hybridization showed that the enhanced expression of CK-M1 expanded from the head to the whole body of larvae as metamorphosis progressed. Quantitative analysis revealed stage-specific high expression of CK-M1 during metamorphosis. The expression level of CK-M1 increased initially and peaked at metamorphosis, decreased afterward, and finally returned to the pre-metamorphosis level. This stage-specific expression pattern suggested strongly that CK-M1 was related to metamorphosis in the Japanese flounder. Its specific role in metamorphosis requires further study. 相似文献
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In this case study, silica concentration, oxygen and strontium isotopes of water samples were used to study surface water–groundwater
interaction at the Xin’an karst water system. The silica concentration in rain water is commonly less than 1 mg/l. In the
areas around the south tributary of the Zhuozhang River, silica concentrations in the groundwater in Quaternary aquifers range
between 4.04 and 7.66 mg/l while that of the surface water varies from 1.49 to 6.9 mg/l. Silica concentrations of most surface
water samples increase with TDS, indicating the effect of groundwater recharge on river water chemistry. On the contour map
of silica concentration of groundwater in Quaternary aquifers, samples located close to surface water often have lower silica
concentrations as a result of surface water recharge. Both overland flow and surface water have impact on karst water according
to our hydrogeochemical study of stable oxygen isotope, Sr isotope and strontium contents. Calculation results of three end
member mixing model show that the contribution of karst water, surface water and overland flow water is 45, 28 and 27%, respectively. 相似文献
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Chunmei Li Xubo Wang Quanqi Zhang Zhigang Wang Jie Qi Qilin Yi Zhipeng Liu Yanan Wang Haiyang Yu 《中国海洋大学学报(英文版)》2012,11(1):32-44
Major histocompatibility complex class II antigens are important in vertebrate immune system.In the present study,the full cDNA sequence of class II A gene was synthesized by RACE-PCR from half-smooth tongue sole(Cynoglossus semilaevis),and its open reading frame(ORF) polymorphism was studied.The whole cDNA sequence was 992 bp in length,including the ORF with 717 bp.Twenty-five alleles were identified and clustered into two distinct groups according to the specific nucleotides/amino acids in specific positions.Eleven alleles belonged to Cyse-DAA while fourteen alleles belonged to Cyse-DBA.Four Cyse-DAA alleles were observed in one individual,and three to five Cyse-DBA alleles were observed in each of the three detected individuals,which indicated that at least two loci existed in each gene.Moreover,in order to study the function of the alleles in resistance to infection,200 individuals were intraperitoneally injected with Vibrio anguillarum and the first 20 dead individuals and 20 surviving ones were selected for genotype analysis.Fifty-six alleles were identified among the 40 individuals.Twenty-nine alleles belonged to Cyse-DAA and the other 27 alleles belonged to Cyse-DBA.Eighteen alleles were selected for studying their function in resistance to infection.Alleles Cyse-DAA*0201,Cyse-DAA*1101,Cyse-DBA*0401,Cyse-DBA*1102,Cyse-DBA*1801 and Cyse-DBA*2201 were identi-fied only in surviving individuals,while alleles Cyse-DAA*0901,Cyse-DBA*1101 and Cyse-DBA*1401 occurred more frequently in dead individuals.This study confirmed the existence and polymorphism of two class II A genes as well as the relationship between alleles of class II A genes and disease susceptibility/resistance in half-smooth tongue sole. 相似文献
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Yongping Liang Xubo Gao Chunhong Zhao Chunlei Tang Haoyong Shen Zhiheng Wang Yanxin Wang 《Hydrogeology Journal》2018,26(5):1371-1385
In Northern China, karst systems in widely distributed carbonate rocks are one of the most important water supplies for local inhabitants. Constrained by the specific geological and geomorphological conditions, most karst water in this region is discharged as individual or groups of springs. This paper summarizes the characteristics, chemistry, and environmental quality of these karst systems in Northern China. Five structural models of karst water systems were identified based on the relationships between the karst geological strata and karst groundwater flow fields. These specific structural models may closely relate to the attendant environmental geological issues and consistent risks from pollution. Over the past 40 years, the karst water systems in Northern China have suffered from various environmental problems, including deteriorating water quality, the drying up of springs, a continuous decline in the level of karst water, and so on. Based on the field investigation and previous data, a preliminary summary is provided of the environmental problems related to the development and evolutionary trends of karst water in this region. The results highlight the significant challenges associated with karst water, and it is essential that all segments of society be made aware of the situation in order to demand change. In addition, the study provides a scientific basis for the management, protection, and sustainable utilization of karst water resources. 相似文献
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岷江上游某水电站工程边坡软岩的崩解特性研究 总被引：2，自引：0，他引：2
工程边坡内软岩分布较广,可区分为泥化夹层、煤、炭质页岩、泥质粉砂岩等4种典型岩组。软岩的发育特征、空间展布形态、崩解特性直接关系到边坡整体稳定性和支护措施的方案设计。在重点研究F3断层、L9、L10、Lc、L11等软带内所发育的几种典型软岩岩组的崩解特性后,获知该类软岩极易吸水,遇水后发生泥化、软化和崩解。通过循环崩解试验,发现工程区内软岩的崩解度与泥质含量和崩解次数具有很好的相关性。同时,根据崩解度与崩解物形态,对软岩进行定性划分,分别定出Ⅴ类崩解岩和5种崩解破坏形式。最后就崩解机理作进一步地深入探讨。该成果为指导类似的工程边坡软岩的崩解性试验研究提供新的思路。 相似文献