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学者姓名：肖爱芳
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Abstract ：
The magma sources, origins and precise forming ages of the miarolite from Qishan and Kuiqi intrusions are still uncertain. New results reveal that, miarolites from the Qishan and Kuiqi intrusions yield crystallization ages of -101 and similar to 98 Ma, and they have a high formation temperature (similar to 910 degrees C) and low oxygen fugacity value, indicating crystallization condition at low pressure in the upper crust with temperature of 678 degrees C. The Qishan and Kuiqi miarolites are characterized by enrichment in SiO2 and high-K alkali, depletion in Ca and Mg, and belong to the high-K weak peraluminous rock series. The samples are enriched in HFSEs (i.e., Ta, Zr and Hf) and LILEs (i.e., Ba, P and Sr), depleted in Ba and Sr with the negative anomaly of Eu. In the primitive mantle normalized trace element spider diagram, the samples show a right-inclined 'seagull-type' pattern, combined the ratios of (La/Yb)N, 10000 x Al/Ga, Rb/Nb and Nb/Ta etc., they were proved to be alkaline A-type granite. Combined the characterize of the trace elements, they were derived from clay-rich source accompanied pelite melting, and subjected to K-feldspar crystallization fractional. The values of eHf(t) and tDM2 are distributed in the range of -2.8 to 3.3 with similar to 1.2 Ga, and -6.0 to 4.0 with similar to 1.2 Ga, revealing that they were generated from the Mesoproterozoic Cathaysia basement rocks. The comprehensive research reveals the Kuiqi and Qishan intrusions derived from crust-mantle mixing and partial melting of the crust, respectively, resulting from lithospheric extension generated by the Paleo-Pacific Plate subducted into the European-Asian Plate.
Keyword ：
A-type granitoid A-type granitoid extension extension geochronology geochronology Mesozoic Mesozoic Southeast China Southeast China subduction subduction
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| GB/T 7714 | Xie, Qifeng , Dong, Yunpeng , Cai, Yuanfeng et al. The Origin of Mesozoic A-type Granitoids, Fujian Province, Southeast China: Insights from Geochronology, Mineralogy and Geochemistry [J]. | ACTA GEOLOGICA SINICA-ENGLISH EDITION , 2024 , 98 (3) : 630-640 . |
| MLA | Xie, Qifeng et al. "The Origin of Mesozoic A-type Granitoids, Fujian Province, Southeast China: Insights from Geochronology, Mineralogy and Geochemistry" . | ACTA GEOLOGICA SINICA-ENGLISH EDITION 98 . 3 (2024) : 630-640 . |
| APA | Xie, Qifeng , Dong, Yunpeng , Cai, Yuanfeng , Zhai, Mingguo , Xiao, Aifang , Zhang, Hong . The Origin of Mesozoic A-type Granitoids, Fujian Province, Southeast China: Insights from Geochronology, Mineralogy and Geochemistry . | ACTA GEOLOGICA SINICA-ENGLISH EDITION , 2024 , 98 (3) , 630-640 . |
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Late Mesozoic mafic dykes, which are widely developed in the North Qinling Orogenic Belt (NQOB), include abundant geodynamic information. This paper describes the mafic dykes that intrude the Late Jurassic granite in the Dayu and Kuyu areas, and reports important petrological constraints for the late Mesozoic tectonic transition from compression to extension in the NQOB. Three zircon U-Pb results show that the minimum ages of the mafic dykes are 139.8 +/- 1.4 Ma, 137.4 +/- 1.7 Ma and 133.4 +/- 0.9 Ma, indicating that the emplacement age of the Dayu and Kuyu mafic dykes is 140-133 Ma. Petrogeochemical analyses suggest that the mafic dykes belong to the high-K calc-alkaline shoshonite series with low SiO2 (46.93-56.73 wt%), MgO (1.88-9.10 wt%) and TiO2 (1.17-1.82 wt%), and high Al2O3 (13.98-17.46 wt%), TFe2O3 (7.81-10.92 wt%) and K2O (1.28-4.78 wt%). The mafic dykes are enriched in large ion lithophile elements (e.g. Rb, Ba, K, La, Sr) and depleted in high-field-strength elements (e.g. Nb, Ta, Zr, Ti). These samples have the right-sloping chondrite-normalised rare earth element patterns, which suggest light rare earth element enrichment and heavy rare earth elements depletion with no obvious Eu anomalies (delta Eu = 0.94-1.11). The I-Sr, epsilon(Nd)(t), epsilon(Hf) (t) and T-DM2(crust) values are 0.7056-0.7060, -10.60 to -5.98, -14.1 to -2.8, and 1382.4 +/- 25.1 to 2081.9 +/- 47.6 Ma, respectively. Both elemental and isotopic geochemistry show that the formation of Dayu and Kuyu mafic dykes is due to the partial decompression melting of previously enriched lithospheric mantle during a delamination process. The mafic dykes have undergone fractionation crystallisation of Mg-Fe phase minerals during magma ascent, accompanied by some crustal contamination. Combined with the regional tectonic setting, we suggested that the NQOB experienced intra-continental extension during the Early Cretaceous.
Keyword ：
delamination delamination Early Cretaceous Early Cretaceous mafic dykes mafic dykes North Qinling Orogenic Belt North Qinling Orogenic Belt Paleo-Pacific Plate subduction Paleo-Pacific Plate subduction partial melting partial melting
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| GB/T 7714 | Huang, Y. N. , Li, D. P. , Xiao, A. F. et al. Petrogenesis and tectonic setting of Early Cretaceous mafic dykes in the North Qinling Orogenic Belt, central China: constraints on the lithospheric lower crust delamination [J]. | AUSTRALIAN JOURNAL OF EARTH SCIENCES , 2023 , 70 (4) : 567-584 . |
| MLA | Huang, Y. N. et al. "Petrogenesis and tectonic setting of Early Cretaceous mafic dykes in the North Qinling Orogenic Belt, central China: constraints on the lithospheric lower crust delamination" . | AUSTRALIAN JOURNAL OF EARTH SCIENCES 70 . 4 (2023) : 567-584 . |
| APA | Huang, Y. N. , Li, D. P. , Xiao, A. F. , Xu, S. M. . Petrogenesis and tectonic setting of Early Cretaceous mafic dykes in the North Qinling Orogenic Belt, central China: constraints on the lithospheric lower crust delamination . | AUSTRALIAN JOURNAL OF EARTH SCIENCES , 2023 , 70 (4) , 567-584 . |
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The North Qinling Orogenic Belt (NQOB) is a composite orogenic belt in central China. It started evolving during the Meso-Neoproterozoic period and underwent multiple stages of plate subduction and collision before entering intra-continental orogeny in the Late Triassic. The Meso-Cenozoic intra-continental orogeny and tectonic evolution had different responses in various terranes of the belt, with the tectonic evolution of the middle part of the belt being particularly controversial. The granites distributed in the Dayu and Kuyu areas in the middle part of the NQOB can provide an important window for revealing the geodynamic mechanisms of the NQOB. The main lithology of Dayu and Kuyu granites is biotite monzogranite, and the zircon U-Pb dating yielded intrusive ages of 151.3 & PLUSMN; 3.4 Ma and 147.7 & PLUSMN; 1.5 Ma, respectively. The dates suggest that the biotite monzogranite were formed at the end of the Late Jurassic. The whole-rock geochemistry analysis shows that the granites in the study areas are characterized by slightly high SiO2 (64.50-68.88 wt%) and high Al2O3 (15.12-16.24 wt%) and Na2O (3.55-3.80 wt%) contents. They are also enriched in light rare earth elements, large ion lithophile elements (e.g., Ba, K, La, Pb and Sr), and depleted in high field strength elements (HFSEs) (e.g., Ta, Nb, P and Ti). Additionally, the granites have weakly negative-slightly positive Eu anomalies (& delta;Eu = 0.91-1.19). Zircon Lu-Hf isotopic analysis showed & epsilon;Hf(t) = -6.1--3.8, and the two-stage model age is T2DM(crust) = 1.5-1.6 Ga. The granites in the study areas are analyzed as weak peraluminous high-K calc-alkaline I-type granites. They formed by partial melting of the thickened ancient lower crust, accompanied by the addition of minor mantle-derived materials. During magma ascent, they experienced fractional crystallization, with residual garnet and amphibole for a certain proportion in the magma source region. Comprehensive the geotectonic data suggest that the end of the Late Jurassic granite magmatism in the Dayu and Kuyu areas represents a compression-extension transition regime. It may have been a response to multiple tectonic mechanisms, such as the late Mesozoic intra-continental southward subduction of the North China Craton and the remote effect of the Paleo-Pacific Plate subduction. image
Keyword ：
I-type granite I-type granite Late Jurassic Late Jurassic North Qinling Orogenic Belt North Qinling Orogenic Belt partial melting partial melting tectonic transition tectonic transition
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| GB/T 7714 | Huang, Yanna , Li, Dunpeng , Xiao, Aifang et al. Geochronology, Petrogenesis and Tectonic Setting of the Late Jurassic I-type Granites in the North Qinling Orogenic Belt, Central China [J]. | ACTA GEOLOGICA SINICA-ENGLISH EDITION , 2023 , 97 (4) : 1132-1149 . |
| MLA | Huang, Yanna et al. "Geochronology, Petrogenesis and Tectonic Setting of the Late Jurassic I-type Granites in the North Qinling Orogenic Belt, Central China" . | ACTA GEOLOGICA SINICA-ENGLISH EDITION 97 . 4 (2023) : 1132-1149 . |
| APA | Huang, Yanna , Li, Dunpeng , Xiao, Aifang , Xu, Songming . Geochronology, Petrogenesis and Tectonic Setting of the Late Jurassic I-type Granites in the North Qinling Orogenic Belt, Central China . | ACTA GEOLOGICA SINICA-ENGLISH EDITION , 2023 , 97 (4) , 1132-1149 . |
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Shanzhuping deposit is located in the southwestern Zijinshan ore field, Shanghang County, Fujian Province, develops the Au, Cu and Mo elements anomaly, and forms Au and Cu deposit. The granodiorite and monzogranite are selected for carrying on petrology, petrography, whole rock geochemistry, U-Pb geochronology and Lu-Hf isotope. Here we report the monzogranite and granodiorite Pb-206/U-238 weighted mean age at 105. 2Ma and 113. 4Ma. Combined with the zircon characteristics of magma oscillation and Th/U ratios, which reveals that there are two episodes magmatic activities of Late Yanshanian. The granodiorite and monzogranite share geochemical affinities with typical island arc, enriched Na element ( Na2O/K2O > 1), light rare earth element ( LREE), large icon lithophile element ( LIEE, such as Ba and K), and U, Th and Pb etc., depleted high field strength element ( HESE, such as Nb, Ta and Zr), and characterized with peraluminous ( A/CNK with 1. 19 similar to 1.68), medium ( La/Yb) N ( 13. 6 similar to 17. 4), and high Mg-#(45. 89 similar to 48. 53); slightly negative Eu anomaly (delta Eu ranges 0. 79 to 0. 97), and slightly positive Ce anomaly ( ranges 1. 0 similar to 1.08). The peak value of zircon two -stage Hf model age (t(DM2)) ranges of 1.05 similar to 1. 10Ga and 0.95 similar to 1. OGa, the epsilon(Hf)( t) ranges of -4. 47 similar to +2.38 ( mainly negative values) and -2. 73 similar to +1.47 (mainly positive values), respectively. Based on previous research results and opinions of this study, we infer that monzogranite derived from melting of Mesoproterozoic ancient basement in upper crust, while granodiorite derived from the Neoproterozoic crustal material and subjected to the contamination of mantle materials. The Shanzhuping deposit formed in Late Yanshanian island arc or active continent margin tectonic setting, which is closely related to paleoPacific plate subducted to Eurasian plate, and the southwest or south of which was predicted as two favorable exploration region.
Keyword ：
Early Cretaceous Early Cretaceous Fujian Province Fujian Province Magmatism Magmatism Shanzhuping deposit Shanzhuping deposit Zijinshan ore field Zijinshan ore field
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| GB/T 7714 | Xie QiFeng , Dong YunPeng , Cai YuanFeng et al. The Early Cretaceous magmatism and geological implication of Shanzhuping deposit in Shanghang region, Zijinshan ore field, Fujian Province, Southeast China [J]. | ACTA PETROLOGICA SINICA , 2022 , 38 (10) : 3037-3051 . |
| MLA | Xie QiFeng et al. "The Early Cretaceous magmatism and geological implication of Shanzhuping deposit in Shanghang region, Zijinshan ore field, Fujian Province, Southeast China" . | ACTA PETROLOGICA SINICA 38 . 10 (2022) : 3037-3051 . |
| APA | Xie QiFeng , Dong YunPeng , Cai YuanFeng , Zhai MingGuo , Xiao AiFang , Zhang Hong et al. The Early Cretaceous magmatism and geological implication of Shanzhuping deposit in Shanghang region, Zijinshan ore field, Fujian Province, Southeast China . | ACTA PETROLOGICA SINICA , 2022 , 38 (10) , 3037-3051 . |
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单竹坪矿床位于福建省上杭县紫金山矿田的西南部,形成了 Au、Cu和Mo 异常,其中Au、Cu富集成矿.选取单竹坪矿床钻孔岩芯中二长花岗岩和花岗闪长岩作为研究对象,开展岩石学、岩相学、全岩地球化学、锆石U-Pb年代学和Lu-Hf同位素研究.研究结果表明,二长花岗岩和花岗闪长岩锆石206Pb/238U加权平均年龄分别为105.2Ma和113.4Ma.二长花岗岩和花岗闪长岩具有富钠(Na2O/K2O＞1),过铝质(A/CNK=1.19～1.68),富集轻稀土(LREE)、大离子亲石元素(LIEE,如Ba、K)和Th、U、Pb和Hf等元素,亏损高场强元素(如Nb、Ta和Ti等)的特征,属于高钾钙碱性过铝质岩石系列,具有岛弧岩浆岩特征.同时具有中等的(La/Yb)N值(13.6～17.4),高Mg#值(45.89～48.53),以及Eu弱负异常(δEu=0.79～0.97)和Ce弱正异常(δCe=1.0～1.08).锆石两阶段Hf模式年龄(tDM2)峰值分别处于0.95～1.0Ma和1.05～1.10Ma区间;εHf(t)值分别介于-4.47～+2.38和-2.73～+1.47,二长花岗岩以负值为主,花岗闪长岩正负值均有.综合研究认为,二长花岗岩来源于中元古界未受幔源组分影响的古老基底地壳熔融而成,花岗闪长岩来源于新元古界地壳物质并经历了壳-幔混合作用;单竹坪矿床形成于燕山晚期岛弧或活动大陆边缘构造环境,与古太平洋板块的俯冲相关,其西南部或南部是成矿远景区.
Keyword ：
单竹坪矿床 单竹坪矿床 岩浆作用 岩浆作用 早白垩世 早白垩世 福建省 福建省 紫金山矿田 紫金山矿田
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| GB/T 7714 | 谢其锋 , 董云鹏 , 蔡元峰 et al. 福建上杭单竹坪矿床早白垩世岩浆作用及地质意义 [J]. | 岩石学报 , 2022 , 38 (10) : 3037-3051 . |
| MLA | 谢其锋 et al. "福建上杭单竹坪矿床早白垩世岩浆作用及地质意义" . | 岩石学报 38 . 10 (2022) : 3037-3051 . |
| APA | 谢其锋 , 董云鹏 , 蔡元峰 , 翟明国 , 肖爱芳 , 张红 et al. 福建上杭单竹坪矿床早白垩世岩浆作用及地质意义 . | 岩石学报 , 2022 , 38 (10) , 3037-3051 . |
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利用1992—2017年7个时期的遥感数据,基于遥感生态指数(RSEI),对福建紫金矿区开采以来的生态质量进行评价.结果表明:1)RSEI可以较好反映矿区生态状态的时空变化,1992—2017年,紫金矿重点开发区内裸土面积逐渐扩大,RSEI呈现略微的下降趋势,但整个区域的RSEI反而有一定程度的上升,重点开发区外围的生态状况出现好转;2)从面积上看,占主导地位的区域RESI由"中等"向"优良"发展,说明紫金矿业集团在开发矿山的同时,注重生态保护;3)紫金山矿区不同时期裸土面积扩张的原因与矿区开发技术和金铜价格上涨有关,而矿区生态质量的总体上升与企业和地方政府在生态环境保护方面的大量经费投入密不可分.
Keyword ：
生态质量 生态质量 紫金山矿区 紫金山矿区 遥感生态指数(RSEI) 遥感生态指数(RSEI)
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| GB/T 7714 | 林梦婧 , 汪小钦 , 肖爱芳 et al. 基于遥感生态指数的福建紫金山矿区生态评估 [J]. | 福州大学学报（自然科学版） , 2020 , 48 (2) : 230-235 . |
| MLA | 林梦婧 et al. "基于遥感生态指数的福建紫金山矿区生态评估" . | 福州大学学报（自然科学版） 48 . 2 (2020) : 230-235 . |
| APA | 林梦婧 , 汪小钦 , 肖爱芳 , 王琳 . 基于遥感生态指数的福建紫金山矿区生态评估 . | 福州大学学报（自然科学版） , 2020 , 48 (2) , 230-235 . |
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通过对李坊重晶石矿床重晶石的Sr同位素分析,探讨钡的物质来源.结果显示,重晶石的Rb含量为2.70×10-6～13.41×10-6,Sr含量为520.40×10-6～2166.00×10-6,87Rb/86Sr比值低,87Sr/86Sr比值介于0.71081～0.71180之间,平均值为0.71126,高于同时期海水锶的87 Sr/86 Sr比值,低于壳源锶的87 Sr/86 Sr平均值,表明重晶石的锶来自海水锶与壳源锶的混合.示踪结果显示重晶石的钡主要来源于下伏地层,并暗示基底属于大陆型地壳.
Keyword ：
成矿物质来源 成矿物质来源 李坊 李坊 福建省 福建省 重晶石矿床 重晶石矿床 锶同位素 锶同位素
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| GB/T 7714 | 陈宪 , 黎敦朋 , 崔碧云 et al. 福建李坊重晶石矿床锶同位素组成及成因意义 [J]. | 福州大学学报（自然科学版） , 2020 , 48 (3) : 404-410 . |
| MLA | 陈宪 et al. "福建李坊重晶石矿床锶同位素组成及成因意义" . | 福州大学学报（自然科学版） 48 . 3 (2020) : 404-410 . |
| APA | 陈宪 , 黎敦朋 , 崔碧云 , 肖爱芳 . 福建李坊重晶石矿床锶同位素组成及成因意义 . | 福州大学学报（自然科学版） , 2020 , 48 (3) , 404-410 . |
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地质认识实习课程是资源勘查工程专业的必修课,是本科生步入地质学科的第一次野外实习,其教学效果对学生今后的专业学习和专业发展具有重要的影响.根据新工科人才培养要求,结合福州大学课程建设和教学改革要求,力图改变传统教学模式,在教学内容和教学方法方面实施改革,以期进一步提升野外地质实践教学质量,培养高素质地学人才.
Keyword ：
地质认识实习 地质认识实习 课程改革 课程改革 资源勘查工程 资源勘查工程
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| GB/T 7714 | 林木森 , 李晓敏 , 肖爱芳 . 新工科背景下地质实习类课程教学改革研究——以地质认识实习课程为例 [J]. | 大学教育 , 2020 , (11) : 88-90 . |
| MLA | 林木森 et al. "新工科背景下地质实习类课程教学改革研究——以地质认识实习课程为例" . | 大学教育 11 (2020) : 88-90 . |
| APA | 林木森 , 李晓敏 , 肖爱芳 . 新工科背景下地质实习类课程教学改革研究——以地质认识实习课程为例 . | 大学教育 , 2020 , (11) , 88-90 . |
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It is a fast and effective method to evaluate the ecological environment of mining area using remote sensing technology. In this paper, Landsat series data from 1992 to 2017 were used to monitor the change of ecological environment of Zijin Mine, located in the west of Fujian province, China. After radiometric calibration, the normalized difference vegetation indexes (NDVI) of Landsat TM or OLI from 1992 to 2017 were calculated. Based on NDVI data, the change of vegetation coverage of environment around Zijin mountain gold-copper deposit was analyzed. The results indicated that: ( 1) The area of Zijin mountain gold-copper deposit was increasing from 1992-2017. During 1996-2001, the area of mine was increasing rapidly because of large-scale blasting for removing loading strata in 1997, and it became obviously larger from 2014-2017 due to the copper price increases. (2)the NDVI around Zijin mountain raised from 1992 to 2014, indicating a better vegetation recovery, but it reduced from 2014 to 2017, indicating a worse vegetation recovery. low NDVI mainly exist in the middle of Zijin deposit, which is relate to mining activities. These results can give some scientific references for assessment of Zijin gold-copper deposit ecological environment.
Keyword ：
NDVI NDVI temporal and spatial variation temporal and spatial variation Zijin gold-copper deposit Zijin gold-copper deposit
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| GB/T 7714 | Lin, Mengjing , Wang, Xiaoqin , Xiao, Aifang . ANALYSIS OF VEGETATION VARIATION AROUND ZIJINSHAN GOLD AND COPPER MINE, FUJIAN, CHINA [C] . 2019 : 6471-6474 . |
| MLA | Lin, Mengjing et al. "ANALYSIS OF VEGETATION VARIATION AROUND ZIJINSHAN GOLD AND COPPER MINE, FUJIAN, CHINA" . (2019) : 6471-6474 . |
| APA | Lin, Mengjing , Wang, Xiaoqin , Xiao, Aifang . ANALYSIS OF VEGETATION VARIATION AROUND ZIJINSHAN GOLD AND COPPER MINE, FUJIAN, CHINA . (2019) : 6471-6474 . |
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The Lifang barite deposit in Fujian province is a large-scale independent barite deposit discovered in the southeastern coastal areas in China. It plays an important role in the sedimentary barite deposits with a more than thirty years mining history, although its genesis and mineralization epoch are still disputed. This paper undertook investigation of ore structure, electron microprobe analyses and fluid inclusion temperature measurement for barite from the Lifang barite deposit in Fujian province. The following findings and cognition are obtained: The hydrothermal exhalative channel phases such as tube structures, breccia structures and honeycomb structures in barite ore were found for the first time. The hyalophane mineral in barite ore with indicative feature of hydrothermal sedimentary genesis was found for the first time. 140 fluid inclusions data yielded the homogenization temperature of fluid inclusion ranging from 89.3 to 208.5, with an average of 162.7, indicating that the Lifang barite deposit belongs to a low temperature hydrothermal sedimentary deposit. Based on evidence such as ore structure, mineralogy and fluid inclusion temperature measurement, this proposed a new cognition that the Lifang barite deposit is a 'white chimney' hydrothermal sedimentary deposit. This understanding provides new important information for the study and prospecting exploration for the early Paleozoic hydrothermal deposits in South China. © 2019, Science Press. All right reserved.
Keyword ：
Barite Barite Deposits Deposits Electron probe microanalysis Electron probe microanalysis Honeycomb structures Honeycomb structures Mineralogy Mineralogy Ore deposits Ore deposits Sedimentology Sedimentology Temperature Temperature Temperature measurement Temperature measurement
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| GB/T 7714 | Li, Dunpeng , Luo, Kun , Xiao, Aifang et al. The new cognition of the genesis of the Lifang barite deposit in Fujian province: Evidence from ore structure, mineralogy and fluid inclusions [J]. | Acta Geologica Sinica , 2019 , 93 (12) : 3095-3110 . |
| MLA | Li, Dunpeng et al. "The new cognition of the genesis of the Lifang barite deposit in Fujian province: Evidence from ore structure, mineralogy and fluid inclusions" . | Acta Geologica Sinica 93 . 12 (2019) : 3095-3110 . |
| APA | Li, Dunpeng , Luo, Kun , Xiao, Aifang , Kong, Lingtian . The new cognition of the genesis of the Lifang barite deposit in Fujian province: Evidence from ore structure, mineralogy and fluid inclusions . | Acta Geologica Sinica , 2019 , 93 (12) , 3095-3110 . |
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