Attribution of the Langshan Tectonic Belt: Evidence from zircon U-Pb ages and Hf isotope compositions

This study describes a previously unidentified Neoproterozoic mafic dyke emplaced in the northern flank of the Langshan Tectonic Belt. This dyke intruded into the micaquartz schist of the Zhaertaishan Group, and yielded an age of 908 ± 8 Ma. The youngest U-Pb ages of micaquartz schist from the Zhaertaishan Group in the Langshan area were 1118 ± 33 Ma,1187 ± 3 Ma and 1189 ± 39 Ma,suggesting that the depositional age of the protolith of the schist was between 908 ± 8 Ma and 1118 ± 33 Ma. In addition, 436 U-Pb age data and 155 Lu-Hf isotopic data from six samples in the Langshan Tectonic Belt and one Permian greywacke from the Wuhai area show distinct differences between the northern and southern flanks of the Main Langshan area. The U-Pb ages of the northern flank are primarily Meso-Neoproterozoic; similar ages have not been identified in the southern flank to date.Moreover, two-stage Hf model ages of the northern flank feature three age peaks at ～900 Ma,～1700 Ma and ～2600 Ma; this differs from Hf model ages of the southern flank, which feature one strong age peak at ～2700 Ma. These results suggest that the northern and southern flanks of the Main Langshan area have different geochronologic characteristics and should be divided further. Based on the U-Pb ages and Hf model ages, the northern and southern flanks of the Main Langshan area are named the North and South Langshan Tectonic Belts. Comparison of the U-Pb age and two-stage Hf model age distributions from the North Langshan Tectonic Belt, South Langshan Tectonic Belt, Alxa Block and the North China Craton(NCC) reveal that the North Langshan Tectonic Belt is similar to the Alxa Block and that the South Langshan Tectonic Belt is similar to the NCC. In addition, the zircon U-Pb age of 860 ±7 Ma commonly observed in the Alxa Block was detected in the Permian greywacke from the Wuhai area of the NCC, which suggests that the amalgamation of the North and South Langshan Tectonic belts(i.e.,the amalgamation of the Alxa Block and the NCC), occurred between Devonian and late Permian.

Influence of contamination on banded iron formations in the Isua supracrustal belt, West Greenland: Reevaluation of the Eoarchean seawater compositions

Banded Iron Formations（BIFs） are chemical sediments, ubiquitously distributed in the Precambrian supracrustal belts; thus their trace element compositions are helpful for deciphering geochemical evolution on the Earth through time. However, it is necessary to elucidate factors controlling the whole-rock compositions in order to decode the ancient seawater compositions because their compositions are highly variable. We analyzed major and trace element contents of the BIFs in the 3.8-3.7 Ga Isua supracrustal belt（ISB）, southern West Greenland. The BIFs are petrographically classified into four types：Black-,Gray-, Green-and White-types, respectively. The Green-type BIFs contain more amphiboles, and are significantly enriched in Co, Ni, Cu, Zn, Y, heavy rare earth element（HREE） and U contents. However,their bulk compositions are not suitable for estimate of seawater composition because the enrichment was caused by secondary mobility of metamorphic Mg, Ca and Si-rich fluid, involvement of carbonate minerals and silicate minerals of olivine and pyroxene and/or later silicification or contamination of volcanic and clastic materials. The White-type BIFs are predominant in quartz, and have lower transition element and REE contents. The Gray-type BIFs contain both quartz and magnetite. The Black-type BIFs are dominated by magnetite, and contain moderate to high transition element and REE contents. But,positive correlations of V, Ni, Zn and U contents with Zr contents suggest that involvement of detrital,volcanic and exhalative materials influences on their contents. The evidence for significant influence of the materials on the transition element contents such as Ni in the BIFs indicates the transition element contents in the Archean ocean were much lower than previously estimated. We reconstructed secular variations of V,Co, Zn and U contents of BIFs through time, which show Ni and Co contents decreased whereas V, Zn and U contents increased through time. Especially, the Ni and Co contents drastically decreased in the Mesoarchean rather than around the Great Oxidation Event. On the other hand, the V,Zn and U contents progressively increased from the Mesoarchean to the Proterozoic. Stratigraphical trends of the BIFs show increase in Y/Ho ratios and decrease in positive Eu anomaly upwards, respectively. The stratigraphic changes indicate that a ratio of hydrothermal fluid to seawater component gradually decrease through the deposition, and support the Eoarchean plate tectonics, analogous to the their stratigraphic variations of seafloor metalliferous sediments at present and in the Mesoarchean.

Characteristics of Compositional Migration in Mylonites from the Ductile Shear Zones of the Southern Tancheng-Lujiang Fault Belt, Eastern Anhui Province

On the basis of field geology, three typical ductile shear zones in the southern part of the Tancheng-Lujiang fault belt have been chosen for a detailed study. Altogether ten samples of the tectonites have been collected for this study. The paper is focused on a comprehensive study of the tectonites in the medium-lower horizons of the ductile shear zones. The mineral compositions of the rocks are analyzed with EPMA and some typical whole-rock samples analyzed by chemical and ICP methods. Based on the comprehensive study of the characteristics of the deformation, the mineral assemblages and the changes of chemical composition of the bulk rocks, this paper presents a discussion on the relationship between the volume loss, the fluid flow and compositional changes during mylonitization of the ductile shear zones in this region. Our study shows that there are a large amount of fluids flowing through the shear zones during the process of mylonization, accompanied by the loss of rock volume and migration of elements and components. Modelling calculation results under different saturation conditions of fluids show that the maximum volume loss of the tectonites is about 60% relative to their protolith, while the fluid/rock ratio ranges from 10 to 103 in different ductile shear zones.

Feldspar Lead Isotopic Composition of Granitoids from the Eastern Qinling Orogenic Belt and Their Tectonic Significance

This paper reports 48 feldspar lead isotope analyses from 27 granitic intrusions,which formed from the Late Proterozic to Mesozoic within the Eastern Qinling oregenic belt. Itis found that the granitic rocks of South Qinling are characterized by a strong block-effect anddepletion in U-Pb and Th-Pb, showing that these rocks came from the same lead isotopetectono-geochemical province, while those of North Qinling are characterized by higher U-Pband Th-Pb for Late Proterozoic to Early Paleozoic ones and lower U-Pb and Th-Pb forLate-Palaeozoic and younger ones in their feldspar lead isotopic composition. In the NorthQinling block, lead isotopic signatures reflect that the source of granitic magma had changedsince the Late Palaeozoic. Comparison of feldspar lead isotopic composition between SouthQinling and North Qinling shows that there is marked difference in lead isotopic compositionfor pre-Palaeozoic granitoids, indicating that the South Qinling and the North Qinling blocksbelong to different tectonic units, but the similarities in lead isotopic composition are quiteclear, which indicates that the South Qinling block had been welded with the North Qinlingblock and that the magma sources of both blocks were identical. The analysis provides directevidence for underplating of the continental crust of South Qinling beneath the North Qinlingblock in the continent-continent interaction stage of the Eastern Qinling oregenic belt.

装配式叠合楼板后浇带接缝处细节施工研究

叠合楼板因整体性能好、构造简单、弹性好以及使用便捷等优势在装配式建筑中具有广泛的应用价值,装配式叠合楼板后浇带接缝处因模板与后浇带叠合板存在空隙等导致其存在漏浆通病问题,其不仅影响装配式建筑的整体美观,而且还增加施工成本。鉴于此,以某装配式项目为例,针对传统施工模式下后浇带接缝处存在的漏浆通病,提出在模板底部采取螺杆反吊和利用废钢筋焊接形成自拉加固体系,加固接缝处模板,以此减少叠合板后浇带接缝空隙,控制叠合板后浇带接缝漏浆通病。

大豆玉米带状复合种植技术研究进展

大豆玉米带状复合种植技术是保障我国玉米和大豆产量的一项关键性技术,本文从品种选育、种植模式研究和配套机械设备的研发等方面进行了介绍,提出了大豆玉米带状复合种植生产中存在的问题,并对相应的技术问题进行展望,为后续大豆玉米带状复合种植提供参考。

新疆西准噶尔造山带北部晚石炭世I型花岗岩的岩石地球化学和锆石Hf- O同位素特征:对其岩石成因与构造过程的启示

新疆西准噶尔造山带发育大量的晚古生代侵入岩,但它们的岩浆源区和形成的构造背景仍然存在较大争议。本文对西准噶尔造山带北部阿尔加提山石英二长岩进行了详细的岩石学、地球化学、锆石Hf-O同位素研究,旨在揭示其岩石成因和构造背景,探讨其与地壳生长的关系。两件样品的锆石U-Pb定年结果分别为301.8±1.4 Ma和303.7±3.1 Ma,形成于晚石炭世。阿尔加提山石英二长岩样品含有角闪石,高硅(SiO_(2)=67.8%~68.9%)、富碱(K_(2)O+Na_(2)O=9.36%~9.89%)、具有低的铝饱和指数(A/CNK=0.96~1.00),伴有低的Ga/Al值(2.27~2.34),Rb/Sr值(0.35~0.50),显示出I型花岗岩的特征。同时,这些样品均富集大离子亲石元素和轻稀土,亏损高场强元素(如Nb、Ta和Ti等),和负的Eu异常(δEu=0.72~0.85),类似于典型俯冲相关的岛弧岩浆特征。这些I型花岗岩具有高的、正的锆石ε_(Hf)(t)值(+11.2~+14.5)和年轻的二阶段Hf模式年龄(t_(DM2)=604~392 Ma),以及比地幔值略高的锆石δ^(18)O值(5.73‰~6.51‰)和高的锆石饱和封闭温度(T_(zr)=854~895℃),可能是新生下地壳在高温背景下部分熔融的产物。结合前人在西准噶尔造山带北部发现的晚石炭世早二叠世A1和A2型花岗岩和埃达克质岩墙,本文认为这些高温岩石组合的形成可能与晚石炭世的洋中脊俯冲及其相关板片窗作用有关。在洋脊俯冲背景下,软流圈地幔上涌加热新生下地壳,促使其发生部分熔融形成I和A_(1)和A_(2)型花岗岩。西准噶尔造山带大多数下地壳主要形成于早古生代,表明该地区在显生宙发生了显著的地壳增长。

阻燃输送带火灾早期温度变化与烟气成分研究

为实现带式输送机火灾早期预警,改进滚筒摩擦实验平台并监测阻燃输送带温度。利用质谱(MS)技术,分析钢丝绳芯阻燃输送带在摩擦事故早期的升温规律与烟气成分。研究表明,随着摩擦持续进行,阻燃输送带表面温度分布呈现出较强的对称性,最高温度区域逐渐向输送带中心集聚,烟气成分随温度变化而改变。根据实验中烟气产物主要成分以及对应的反应过程,将钢丝绳芯阻燃输送带升温过程分为氧化反应阶段(环境温度至100℃)、取代反应阶段(100~160.2℃)和热解反应阶段(160.2℃以后)。当阻燃输送带处于氧化反应阶段时,输送带热容量较小、升温快,产物多为烷基和酯类化合物;取代反应阶段热容量逐渐增加,升温放缓,产物多为硝基、醚类、羧酸类化合物;热解反应阶段输送带内部热容量基本稳定,升温速率最小,在160.2℃时在烟气成分中首次检测到含氯化合物。

中亚造山带北山南部柳园洋晚古生代两阶段古地理演化

甘蒙北山地区位于中亚造山带中段,其间的柳园洋是古亚洲洋的重要分支之一,关于该洋盆的演化过程存在两阶段裂谷盆地和单阶段长期俯冲两种认识。柳园洋位于北山南部石板山地块和双鹰山地块之间,石板山地块的晚古生代沉积序列和物源变化完整记录了洋盆的古地理演化过程,对于重建区域构造演化有重要意义。此次研究聚焦石板山地块独山地区的上古生界火山-沉积序列,通过砂岩碎屑颗粒组分和碎屑锆石U-Pb-Hf同位素分析,提供柳园洋古地理演化的约束证据。本文数据表明:独山地区下—中泥盆统碎屑锆石年龄为早古生代单峰式分布(~415Ma),来自于柳园洋向南俯冲在石板山地块边缘而形成的岩浆弧;上石炭统—下二叠统样品中出现了明显的中元古代碎屑锆石年龄(~1426Ma),来自于北侧的双鹰山地块和中天山地块,指示洋盆闭合事件;下二叠统碎屑锆石年龄主要为晚石炭世—早二叠世单峰式分布(301~290Ma),来自于裂谷火山活动。此外,本次研究通过对北山南部已发表物源学数据的统计计算,进一步证明并完善了古生代柳园洋两阶段演化模型:中奥陶世—中泥盆世,柳园洋双向俯冲至敦煌-石板山地块和双鹰山地块之下;晚泥盆世,柳园洋闭合,直至石炭纪晚期,敦煌-石板山-双鹰山地块形成了统一的陆缘环境;早—中二叠世,柳园裂谷盆地逐步发育至原洋盆地。

几种土壤封闭处理除草剂对大豆-玉米带状复合种植田杂草防效及安全性的影响

为了探明大豆-玉米带状复合种植模式下的有效化学除草技术,采用室内生测结合田间试验,通过土壤喷雾处理方法,调查除草剂720 g/L异丙甲草胺乳油、70%嗪草酮可湿性粉剂、75%噻吩磺隆水分散粒剂、80%唑嘧磺草胺水分散粒剂、41%氟噻草胺悬浮剂对大豆、玉米的安全性以及在田间的杂草防除效果。结果显示,唑嘧磺草胺、噻吩磺隆、嗪草酮与氟噻草胺、异丙甲草胺两两混用后,田间杂草药后30 d防效达87%以上,药后45 d防效达93%以上,持效期也相对较长。受环境影响,5种除草剂虽在室内试验表现出一定抑制作用,但田间各单剂混用后与对照的表现相差不大,说明对大豆、玉米安全。综上,异丙甲草胺、嗪草酮、噻吩磺隆、唑嘧磺草胺、氟噻草胺单用或混用,可在大豆-玉米带状复合种植田块中于大豆、玉米播种后1~2 d内进行土壤喷雾处理防除杂草。

大豆高粱带状复合机械化精量种植技术

大豆高粱带状复合机械化精量绿色化种植技术,是集覆膜、穴播、覆土一体的带状复合种植栽培管理技术,可实现抗旱、保温、提墒、提高出苗率,降低投入,增加产出的目的。

南通地区夏播大豆玉米带状复合种植品种及密度组合试验研究

为筛选适合南通地区夏播大豆玉米带状复合种植品种及密度,文章对2022年南通地区开展的大豆玉米带状复合种植品种比较试验和种植密度组合试验进行分析。结果表明,南通地区大豆玉米带状复合种植通豆13和江玉877产量水平较高。利用通豆13和苏玉10号进行大豆玉米带状复合种植的最佳株行距组合为:通豆13行距40 cm,株距10 cm;苏玉10号行距40 cm,株距10 cm;通豆13与苏玉10号行距为70 cm。

水系沉积物地球化学“弱小”异常研究——以嵩县幅Au元素异常为例

传统的化探数据处理方法全区常采用统一异常下限圈定异常,存在将异常扩大或者忽略“弱小”异常的缺点,笔者在河南省嵩县地区采用统一的异常下限圈定1∶5万水系沉积物测量综合异常,发现区内Au异常弱小、零散、规律性差。通过采用地质子区异常下限衬值法对区内化探数据重新处理,发现在研究区内存在多个“弱小”异常,这些异常沿主构造方向大致断续分布,具有一定的规律性。通过对“弱小”异常开展查证工作,最终在坡根、七峰山等地发现了多个金矿(化)体。证明在高背景地球化学异常地区采用地质子区异常下限衬值法圈定化探异常并指导找矿具有良好效果,研究成果可为下一步地质找矿工作提供依据。

大豆玉米带状复合种植田杂草防除技术集成试验

为了集成适合大豆玉米带状复合种植田杂草防除的有效技术模式,于2023年开展土壤喷雾封闭、土壤喷雾封闭+茎叶喷雾补杀(“一封一补”)防除杂草的大区试验。结果表明,播后苗前使用80%砜吡草唑·嗪草酮WG 450 g/hm 2或45%精异丙甲草胺CS 1500 mL/hm 2+33%精异草·丙炔氟CS 1500 mL/hm 2进行土壤喷雾,对禾草的株防效在94%以上;45%精异丙甲草胺CS 1500 mL/hm 2+33%精异草·丙炔氟CS 1500 mL/hm 2土壤喷雾、80%砜吡草唑·嗪草酮WG 450 g/hm 2土壤喷雾封闭+480 g/L灭草松AS 3000 mL/hm 2茎叶喷雾对禾草及阔叶杂草的综合防效达94%以上。集成了适合禾草化除的“土壤封闭”模式、禾阔双除的“土壤封闭”模式以及“一封一补”模式,安全性高,在登记的基础上,可用于河南省大豆玉米带状复合种植田杂草防治。土壤喷雾后,必须通过浇水或降雨来增加土壤墒情,才能较好地发挥药效。

半钢轮胎成型机贴合鼓预收缩应用研究

轿车的安全稳定性除了与减震系统有关外,也与轮胎有密切的关系。市场经济的需求对轮胎生产有了更高的要求,冠带变张力的应用提高了轮胎了均动性,提升了轿车行驶中的舒适度。但在实际生产中生产中,成型机出现了胎体复合件塌陷的问题,无法保证胎体与复合件的同心度,造成了均动数据不稳定,本案为了更好稳定产品性能从贴合鼓预收缩功能的使用做了研究。

Geochemistry, geochronology and Hf isotope of granitoids in the Chinese Altai: Implications for Paleozoic tectonic evolution of the Central Asian Orogenic Belt

The Chinese Altai in northwestern Xinjiang has numerous outcrops of granitoids which provide critical information on accretionary orogenic processes and crustal growth of the Central Asian Orogenic Belt.Zircon U-Pb ages, Hf-isotopic compositions and whole-rock geochemistry of monzogranite and granodiorites in the Qinghe County are employed to elucidate Paleozoic tectonics of the Chinese Altai. Granodiorites have crystallization ages of 424.6 ± 3.1 Ma(MSWD = 0.23) and 404.0 ± 3.4 Ma(MSWD = 0.18);monzogranite was emplaced in the early Permian with a crystallization age of 293.7 ± 4.6 Ma(MSWD = 1.06). Both granodiorites and monzogranite are I-type granites with A/CNK ratios of 0.92 -0.97 and 1.03 -1.06, respectively. They also show similar geochemical features of high HREE and Y contents, low Sr contents and Sr/Y ratios, as well as enrichment of Cs, Rb, Th and U, and depletion of Nb, Ta, P and Ti.These geochemical features indicate that the monzogranite and granodiorites were formed in an arc setting related to subduction. The gneissic monzogranites display high SiO_2 and K_2 O contents, and belong to the high-K calc-alkaline series. In the chondrite normalized REE distribution pattern, the monzogranite samples exhibit enrichment of LREE with strong negative Eu anomalies(σE u =0.44 -0.53), zircon εHf(t) values from +7.24 to +12.63 and two-stage Hf model ages of 463 -740 Ma. This suggests that the monzogranite was generated from the mixing of pelitic and mantle material. The granodiorite samples are calc-alkaline granites with lower contents of Si O_2 and Na_2 O + K_2 O, higher contents of TiO_2, Fe_2O_3~t, MgO and CaO compared to the monzogranite samples. They also show enrichment of LREE and moderate negative Eu anomalies(σE u= 0.54 =0.81), as well as slightly higher differentiation of LREE than that of HREE. The425 Ma granodiorite has zircon εHf(t) values from -0.51 to +1.98 and two-stage Hf model ages of 1133 -1240 Ma, whereas the 404 Ma granodiorite displays those of +2.52 to +7.50 and 816 -1071 Ma.Geochemistry and zircon Hf isotopic compositions indicate that granodiorites were formed by partial melting of juvenile lower crust. Together with regional geology and previous data, the geochemical and geochronological data of the monzogranite and granodiorites from this study suggest long-lived subduction and accretion along the Altai Orogen during ca. 425 -294 Ma.

Tourmaline geochemistry and boron isotopic variations as a guide to fluid evolution in the Qiman Tagh W-Sn belt, East Kunlun, China

The Qiman Tagh W-Sn belt lies in the westernmost section of the East Kunlun Orogen, NW China, and is associated with early Paleozoic monzogranites, tourmaline is present throughout this belt. In this paper we report chemical and boron isotopic compositions of tourmaline from wall rocks, monzogranites, and quartz veins within the belt, for studying the evolution of ore-forming fluids. Tourmaline crystals hosted in the monzogranite and wall rocks belong to the alkali group, while those hosted in quartz veins belong to both the alkali and X-site vacancy groups. Tourmaline in the walk rocks lies within the schorl-dravite series and becomes increasingly schorlitic in the monzogranite and quartz veins. Detrital tourmaline in the wall rocks is commonly both optically and chemically zoned,with cores being enriched in Mg compared with the rims. In the Al-Fe-Mg and Ca-Fe-Mg diagrams,tourmaline from the wall rocks plots in the fields of Al-saturated and Ca-poor metapelite, and extends into the field of Li-poor granites, while those from the monzogranite and quartz veins lie within the field of Li-poor granites. Compositional substitution is best represented by the MgFe_(-1), Al(NaR)_(-1), and AlO(Fe(OH))_(-1) exchange vectors. A wider range of δ^(11)B values from -11.1‰ to -7.1‰ is observed in the wall-rock tourmaline crystals, the B isotopic values combining with elemental diagrams indicate a source of metasediments without marine evaporates for the wall rocks in the Qiman Tagh belt. The δ^(11)B values of monzogranite-hosted tourmaline range from -10.7‰ and-9.2‰, corresponding to the continental crust sediments, and indicate a possible connection between the wall rocks and the monzogranite. The overlap in δ^(11)B values between wall rocks and monzogranite implies that a transfer of δ^(11)B values by anataxis with little isotopic fractionation between tourmaline and melts. Tourmaline crystals from quartz veins have δ^(11)B values between -11.0‰ and-9.6‰, combining with the elemental diagrams and geological features, thus indicating a common granite-derived source for the quartz veins and little B isotopic fractionation occurred. Tourmalinite in the wall rocks was formed by metasomatism by a granite-derived hydrothermal fluid, as confirmed by the compositional and geological features.Therefore, we propose a single B-rich sedimentary source in the Qiman Tagh belt, and little boron isotopic fractionation occurred during systematic fluid evolution from the wall rocks, through monzogranite, to quartz veins and tourmalinite.

Geochemical characteristics of the fluid inclusions in the Gangxi Fault Belt, Huanghua Depression, Bohai Bay Basin, China

We studied the geochemical characteristics of the fluid inclusions in the Ordovician carbonates and the Oligocene Shahejie Formation sandstones from 15 wells in the Gangxi Fault Belt, Huanghua Depression. The fluid inclusions are all sec- ondary with gas/liquid ratio of 5%~10%. Base on Raman they are mainly composed of H2O, CO2 and CH4. The homogenization temperatures, combined with burial and geothermal history of the host rock, indicate that the fluid flows in the Shahejie Formation and the Ordovician carbonates were trapped in Neocene. Using a VG5400 mass spectrometer, the helium isotopic compositions were analyzed. Interpretation of results suggested a significant amount of mantle-derived helium mainly accumulating in the intersections of the NWW trending Xuzhuangzi and NE trending Gangxi faults. The maturity of hydrocarbon decreases from the intersection to the outside pointing out that the fluid related to the NWW trending Xuzhuangzi and NE trending Gangxi faults. These factors implied the fluid inclusions have a close relationship to the local tectonic setting. Gangxi Fault Belt experienced intensive Neo-tectonic activities in Cenozoic. Widespread faulted-depressions and strong volcanic eruptions manifested its tec- tonic status of extensional stress field. Mantle uplift caused the movement of magma that carried mantle-derived gases and deep heat flows, the deep-rooted tension faults provided the passages for the gases and heat flows to shallow crust levels.

Geochemistry,geochronology and Hf isotope of granitoids in the northern Alxa region:Implications for the Late Paleozoic tectonic evolution of the Central Asian Orogenic Belt

The tectonic setting of the northern Alxa region during the Late Paleozoic is highly controversial.The key to resolve this controversy is to recognize the Late Paleozoic magmatic processes in the northern Alxa.In this paper,we present new zircon U-Pb ages,Hf-isotopic compositions and whole-rock geochemical data of four granitoids along the Zhusileng-Hangwula Tectonic Belt in the northern Alxa region that could provide critical information about the tectonic evolution of this region.The zircon U-Pb data could be grouped as two phases:Late Devonian granite and diorite(ca.373-360 Ma),and Late Carboniferous granodiorite(ca.318 Ma).The Late Devonian granites and diorites are metaluminous to slightly peraluminous,with A/CNK and A/NK ratios of 0.90-1.11 and0.95-2.19,respectively.The Late Devonian diorites are characterized by high MgO,Cr and Ni contents and MgO#values,together with variableεHf(t)values from-1.0 to+1.3 and old TDM2 ages varied from 1283 Ma to 1426 Ma,indicating the primary magma was potentially derived from magma mixing of depleted mantle with Mesoproterozoic continental crust.Even though the Late Devonian granites yielded most positive and minor negative eHf(t)values between-1.1 to+5.7(three grains are negative)with two-stage model ages(TDM2)of 1003-1438 Ma,they display low MgO,Cr and Ni contents and MgO#values,suggesting that they were mainly derived from juvenile crustal materials,mixed with a small amount of ancient crust.The Late Carboniferous granitoids are metaluminous and medium-K calc-alkaline series,with A/CNK and A/NK ratios ranging from 0.88 to 0.95 and1.75 to 1.90,respectively.These rocks were potentially derived from juvenile crustal materials mixed with depleted mantle,as evidenced by their highεHf(t)values(+11.6 to+14.1)and young TDM2 ages(427 Ma to 586 Ma),as well as high Mg#values,and MgO,Ni and Cr contents.Our data,along with available sedimentary evidence and previous researches,indicate that the Late Devonian and Late Carboniferous rocks are arc-related granitoids under the subduction setting.The identification of arc-related granitoids in the northern Alxa region not only reveals the Late Paleozoic magmatic process in response to the subduction of Paleo Asian Ocean,but also provide significant constrains to the tectonic evolution of the Central Asian Orogenic Belt.

Water-Rock Interactions and Chemical Composi-tional Variations During Ductile Deformation ofthe NW-Striking Shear Zone in the Jiapigou Gold Belt, China

Two kinds of mylonite series rocks, felsic and mafic, have been recognized in the NW-striking shear zone of the Jiapigou gold belt. During ductile deformation, a large amount of fluid interacted intensively with the mylonite series rocks: plagioclases were sericitized and the An values declined rapidly, finally all of them were trans formed to albites; dark minerals were gradually replaced by chlorites （mostly ripidolite）. Meanwhile, large-scale and extensive carbonation also took place, and the carbonatization minerals varied from calcite to dolomite and ankerite with the development of deformation. The δ13C values of the carbonates are - 3. 0‰--5. 6‰ suggesting a deep source of carbon. The ductile deformation is nearly an iso-volume one （fv=1）. With the enhancement of shear deformation, SiO2 in the two mylonite series rocks was depleted, while volatile components such as CO2 and H2O, and some ore-forming elements such as Au and S were obviously enriched. But it is noted that the enrichment of An in both the mylonite series rocks did not reach the paygrade of gold. The released SiO2 from water-rock interactions occurred in the form of colloids and absorbed gold in the fluid. When brittle structures were formed locally in the ductile shear zone, the ore-forming fluids migrated to the structures along micro fractures, and precipitated auriferous quartz because of reduction of pressure and temperature. Fluid inclusion study shows that the temperature and pressure of the ore-forming fluids are 245-292℃ and 95.4-131. 7MPa respectively; the salinity is 12. 88-16. 33 wt% NaCl; the fluid-phase is rich in Ca2+, K+, Na+, Mg2+, F- and Cl-, while the gaseous phases are rich in CO2 and CH4. The δDand δ18 O values of the ore-forming fluid are - 84. 48‰- - 91. 73‰ and - 0. 247‰-+2.715‰ respectively, suggesting that the fluid is composed predominantly of meteoric water.