Chemie Der Erde-Geochemistry最新文献

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Positive Matrix Factorization (PMF) based on geochemical data for revising geological map in semi-desert covered terrains: A case study from a map sheer of Urat Rear Banner, Inner Mongolia, China 基于地球化学数据的正矩阵分解(PMF)方法在半荒漠覆盖地区修正地质图——以内蒙古乌拉特后旗地图为例
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-05-03 DOI: 10.1016/j.chemer.2025.126299
Yanling Sun, Xueqiu Wang, Hanliang Liu, Jian Zhou, Mingjun Xie
{"title":"Positive Matrix Factorization (PMF) based on geochemical data for revising geological map in semi-desert covered terrains: A case study from a map sheer of Urat Rear Banner, Inner Mongolia, China","authors":"Yanling Sun,&nbsp;Xueqiu Wang,&nbsp;Hanliang Liu,&nbsp;Jian Zhou,&nbsp;Mingjun Xie","doi":"10.1016/j.chemer.2025.126299","DOIUrl":"10.1016/j.chemer.2025.126299","url":null,"abstract":"<div><div>There is a significant deficiency for geological mapping in the Gobi Desert terrain covered by wind-blown sands with limited exposure of bedrock. Major and minor element data of stream sediments using Positive Matrix Factorization (PMF) analysis were employed to interpret the geological signatures from the Urat Rear Banner, a representative area of the Gobi Desert terrains. Six primary geochemical factors (M1, M2, M3, T1, T2, T3), corresponding to geological units were extracted from 8 major elements and 18 minor elements. Notably, the SiO<sub>2</sub>-Al<sub>2</sub>O<sub>3</sub>-K<sub>2</sub>O-and Pb-Ba-Th-Be-Y-Li-U combinations (primarily M1 and T1) are associated with felsic intrusive rocks, complex metamorphic rocks, and sandstones. The MgO-Fe<sub>2</sub>O<sub>3</sub>-TiO<sub>2</sub>, Cu-Mn-Zn-Co combinations (primarily M2 and T2) indicate basic intrusive rocks, complexes. The Al<sub>2</sub>O<sub>3</sub>-Na<sub>2</sub>O-CaO, Sr-Co-Mn-P-Cu-Zn-Ba (primarily M3 and T3) are related to neutral intrusive bodies (or complexes) and marble (or limestone). Additionally, the study utilizes standardized M1, M2, and M3 factor scores to refine the delineation of lithological boundaries of magmatic rocks. The findings highlight the effectiveness of the PMF method coupled with stream sediment geochemistry, as a powerful tool for extracting geological signatures. This approach offers valuable insights into geological information extraction in Gobi Desert terrains, particularly for identifying and delineating lithological boundaries within magmatic rock formations.</div></div>","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126299"},"PeriodicalIF":2.6,"publicationDate":"2025-05-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143911632","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Petrogenetic and dynamic links between felsic and mafic magmas: Insights from the Devonian post-collisional magmatism in the North Qaidam terrane, western China 柴达木北缘泥盆系碰撞后岩浆活动的启示——长英质岩浆与镁质岩浆的成因与动力学联系
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-04-28 DOI: 10.1016/j.chemer.2025.126298
Denghui Chen , Hao Wu , Dongdong Yan , Chengxiang Li , Huajun Wen , Fuhao Xiong
{"title":"Petrogenetic and dynamic links between felsic and mafic magmas: Insights from the Devonian post-collisional magmatism in the North Qaidam terrane, western China","authors":"Denghui Chen ,&nbsp;Hao Wu ,&nbsp;Dongdong Yan ,&nbsp;Chengxiang Li ,&nbsp;Huajun Wen ,&nbsp;Fuhao Xiong","doi":"10.1016/j.chemer.2025.126298","DOIUrl":"10.1016/j.chemer.2025.126298","url":null,"abstract":"<div><div>Felsic-mafic magmatism in post-collisional settings provides valuable insights into the growth and evolution of continental crust, but the interaction processes between felsic and mafic magmatism and their implications for the diversity of igneous rocks remain controversial. This study presents petrological, geochronological, geochemical, and Sr-Nd-Hf isotopic analyses of the Mohe felsic-mafic complex, a rare post-collisional composite pluton in the North Qaidam terrane (western China), to investigate the petrogenetic and dynamic links between felsic and mafic magmas. The results reveal that the Mohe complex, consisting of granite, granodiorite, diorite, and appinites, is genetically related and formed between ca. 408–400 Ma. The granites and granodiorites are classified as I-type and are characterized by enriched isotopic signatures, including whole-rock (<sup>87</sup>Sr/<sup>86</sup>Sr)ᵢ values of 0.714584–0.728765, εNd<sub>(400 Ma)</sub> values of −7.75 to −5.56, and zircon εHf(t) values of −3.04 to −0.28. These rocks were primarily derived from partial melting of Mesoproterozoic to Paleoproterozoic crustal materials, with minor input from a mantle source. The appinites display depleted zircon Hf isotopic compositions (εHf(t) = +4.10 to +5.71), indicating derivation from an OIB-like depleted mantle source that was metasomatized by subducted slab-derived melts. The diorites show weakly enriched isotopes ((<sup>87</sup>Sr/<sup>86</sup>Sr)<sub><em>i</em></sub> = 0.709358–0.713210, εNd<sub>(400 Ma)</sub> = −2.99 to −2.73, εHf(t) = −1.35 to +3.54), and were formed by the mixing of 80–90 % appinitic magma with 10–20 % crustal-derived granitic magma. Our findings suggest that the Early Devonian magmatism in the North Qaidam terrane was likely driven by slab break-off-related geodynamic processes, where crust-mantle magma mixing, along with mineral accumulation and fractional crystallization, played a key role in the petrological diversity of the continental crust in a post-collisional extensional setting.</div></div>","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126298"},"PeriodicalIF":2.6,"publicationDate":"2025-04-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143911631","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Enhanced analysis of hydrothermal alteration and mineral prospecting through integration of ASTER and aeroradiometric data: A case study from the Ouarzazate region, Morocco 结合ASTER和航空辐射数据加强热液蚀变分析和找矿:以摩洛哥瓦尔扎扎特地区为例
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-04-26 DOI: 10.1016/j.chemer.2025.126296
Ilham El Hakimi, Lahsen Achkouch, Younesse El Cheikh, Mohammad Taadid, Houda Bourouda, Ahmed Rachid, Ahmed Attou
{"title":"Enhanced analysis of hydrothermal alteration and mineral prospecting through integration of ASTER and aeroradiometric data: A case study from the Ouarzazate region, Morocco","authors":"Ilham El Hakimi,&nbsp;Lahsen Achkouch,&nbsp;Younesse El Cheikh,&nbsp;Mohammad Taadid,&nbsp;Houda Bourouda,&nbsp;Ahmed Rachid,&nbsp;Ahmed Attou","doi":"10.1016/j.chemer.2025.126296","DOIUrl":"10.1016/j.chemer.2025.126296","url":null,"abstract":"<div><div>The study area, situated in the western segment of the Saghro Massif within the Anti-Atlas belt, is characterized by mineralized deposits, intricate lithological formations, and distinctive tectonic features. This research integrates ASTER imagery analysis with gamma-ray spectrometry data to map alteration zones and examine the geochemical and mineralogical processes that influence radioactive element distribution. Specific analytical techniques are applied to investigate relationships among argillic, phyllic, propylitic alterations, iron oxides, and regions with elevated concentrations of radiometric elements. Gamma-ray spectrometry data, including mono-elemental maps of radiometric components (potassium in %, equivalent uranium in ppm, and equivalent thorium in ppm), are analyzed alongside interpreted ASTER images to identify potential mineralization zones. Ratios of K/eU and K/eTh, along with the F parameter, are processed within a fuzzy model framework, which combines these datasets into a comprehensive mineral prospectivity map that serves as a tool for guiding exploration. This analysis identifies four hydrothermal alteration zones as highly promising for mineral exploration, suggesting a likely association between magmatic processes and spatially correlated hydrothermal alteration, thereby supporting further detailed exploration initiatives.</div></div>","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126296"},"PeriodicalIF":2.6,"publicationDate":"2025-04-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143883029","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Geochemistry, zircon UPb ages and Hf isotopes of Tra Bong granitoid from Kontum massif, central Vietnam, and its petrogenetic significance 越南中部Kontum地块特拉峰花岗岩的地球化学、锆石UPb年龄和Hf同位素特征及其成岩意义
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-04-25 DOI: 10.1016/j.chemer.2025.126295
Nguyen Huu Trong , Pham Trung Hieu , Pham Minh , Bui Kim Ngoc , Nguyen Dinh Luyen , To Xuan Ban
{"title":"Geochemistry, zircon UPb ages and Hf isotopes of Tra Bong granitoid from Kontum massif, central Vietnam, and its petrogenetic significance","authors":"Nguyen Huu Trong ,&nbsp;Pham Trung Hieu ,&nbsp;Pham Minh ,&nbsp;Bui Kim Ngoc ,&nbsp;Nguyen Dinh Luyen ,&nbsp;To Xuan Ban","doi":"10.1016/j.chemer.2025.126295","DOIUrl":"10.1016/j.chemer.2025.126295","url":null,"abstract":"<div><div>Tra Bong granitoid, distributed in the northern area of Kontum, primarily consists of diorite and granodiorite. The main rock-forming minerals contain plagioclase (26–60 %), K-feldspar (8–22 %), quartz (15–33 %), biotite (3–7 %), and hornblende (9–20 %). The accessory minerals are sphene, apatite, zircon, and magnetite. Tra Bong granitoids are characterized by SiO<sub>2</sub> (58.83–65.8 %), total alkali (6.68–8.03 %), and A/CNK (0.80–0.90). They show high-K and relative enrichment of large-ion lithophile elements (Sc, Rb, and K), and the relative depletion of Nb, Ta, and Ti elements. The P<sub>2</sub>O<sub>5</sub> content decreases with increasing SiO<sub>2</sub>, and Th increases with Rb, a trend typical of I-type granites. All observed petrographic and geochemical characteristics suggested that the Tra Bong granitoid is typical of the I-type granite, formed in a subduction zone. The U<img>Pb crystallization age ranges from 254.5 to 255.0 Ma, coinciding with the Late Permian-Early Triassic magmatic activity, which was previously reported in the Truong Son belt. The ε<sub>Hf</sub>(t) value together with the Hf zircon model ages (T<sub>DM2</sub>) ranges from 1011 to 1159 Ma. The Tra Bong granitoid is a result of partial melting Mesoproterozoic mafic-intermediate magmatic rocks, with a minor amount of metasedimentary crust remelting. In conjunction with other Permian-Triassic magmatic rocks along Truong Son belt and the Song Ma suture, the Tra Bong granitoid represents magmatic activity related to subduction-collision of the Indochina and South China blocks and closure of Paleo-Tethys Ocean in the Late Permian-Early Triassic, along the Song Ma suture.</div></div>","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126295"},"PeriodicalIF":2.6,"publicationDate":"2025-04-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143895853","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Identifying geochemical element distribution patterns through multiple-point geostatistical simulation and singularity analysis: A case study of the Wulonggou-Balong Area, Qinghai, China 基于多点地质统计模拟和奇异性分析的地球化学元素分布模式识别——以青海乌龙沟-巴龙地区为例
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-04-19 DOI: 10.1016/j.chemer.2025.126294
Mengyu Zhao , Qinglin Xia , Wenjun Li
{"title":"Identifying geochemical element distribution patterns through multiple-point geostatistical simulation and singularity analysis: A case study of the Wulonggou-Balong Area, Qinghai, China","authors":"Mengyu Zhao ,&nbsp;Qinglin Xia ,&nbsp;Wenjun Li","doi":"10.1016/j.chemer.2025.126294","DOIUrl":"10.1016/j.chemer.2025.126294","url":null,"abstract":"<div><div>The identification of geochemical element distribution patterns, the extraction of anomalies from geochemical exploration data, and the analysis of deep-level mineralization information are essential to guiding mineral prospectivity mapping. The spatial distribution of geochemical elements mainly arises from complex geological processes, making it challenging for standard deterministic interpolation techniques to capture its complex structure. In singularity analysis of element distribution, the size and geometric configuration of the sliding window significantly impact the geochemical anomaly distribution. Accordingly, this study incorporated the complex patterns extracted from multi-scale exploration geochemical data into a multiple-point geostatistical simulation framework to characterize geochemical element distributions at a fine scale. Fractal topography and singularity analysis were integrated as key analytical tools to identify and extract anisotropic geochemical anomalies. Stream sediment geochemical data from the Wulonggou–Balong area, Qinghai, China, were used as a case study to delineate gold-related geochemical spatial distribution patterns. The proposed multiple-point geostatistical (MPS) method enhanced anomaly intensity in local regions while achieving higher fidelity in reproducing spatial distribution patterns that align with regional geological trends. The spatial distribution patterns of geochemical anomalies, analyzed through diverse fractal topological relationships, highlight anisotropic characteristics in geochemical element distributions governed by ore-controlling factors. Practical application demonstrated that the methods effectively identify undetected weak anomalies associated with mineralization-favorable zones within gold geochemical distribution patterns and minimize uncertainty in anomaly interpretation.</div></div>","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126294"},"PeriodicalIF":2.6,"publicationDate":"2025-04-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143864650","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Geochronology and petrogenesis of magmatic and high-grade metamorphic rocks in the Eocene Chapedony core complex: New insights into the basement geology of Iran 始新世Chapedony岩浆岩和高变质岩的年代学和岩石成因:伊朗基底地质的新认识
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-04-11 DOI: 10.1016/j.chemer.2025.126290
Zeynab Gharamohammadi , Peter A. Cawood , Ali Kananian , Reza Nozaem , Yona Jacobsen , David Lentz , Jafar Omrani
{"title":"Geochronology and petrogenesis of magmatic and high-grade metamorphic rocks in the Eocene Chapedony core complex: New insights into the basement geology of Iran","authors":"Zeynab Gharamohammadi ,&nbsp;Peter A. Cawood ,&nbsp;Ali Kananian ,&nbsp;Reza Nozaem ,&nbsp;Yona Jacobsen ,&nbsp;David Lentz ,&nbsp;Jafar Omrani","doi":"10.1016/j.chemer.2025.126290","DOIUrl":"10.1016/j.chemer.2025.126290","url":null,"abstract":"&lt;div&gt;&lt;div&gt;The Arabia-Eurasia convergence zone provides an evolving record from oblique subduction to continental collision resulting in multiple transient tectonothermal events. Although the subduction of the Neotethys below the Iranian terranes and its relation to the arc and back-arc magmatism throughout the late Mesozoic and Cenozoic in Iran has been documented, the detailed geochemical and isotopic transition from subduction to back-arc extension was not constrained. This study reports the first evidence into the petrogenesis of magmatic diversity of Chapedony core complex (CCC) and the coexistence of Nb-enriched rocks and adakite-like rocks as a result of old crustal recycling. Integrated study of petrography, whole-rock major- and trace-element geochemical data supported with Sr and Nd isotope compositions, zircon U&lt;img&gt;Pb and traces, and zircon Hf isotope analyses reveal a protracted and pulsed evolution of the CCC. The complex consists of leucosome-bearing gabbro-diorite-granodiorite, quartz diorite, and biotite granite that formed between 50 and 40 Ma, but contains amphibolite (metabasite) bodies with zircon cores yielding U&lt;img&gt;Pb ages of 518 Ma and 189 Ma with MORB- and OIB-like characteristics, respectively. Biotite granites are divisible into two types; Type 1 have zircons with a wide range ages, while Type 2 are biotite granites with Eocene ages and lack inherited zircons. Biotite granites Type 1 yield a range of zircon ages (45–3200 Ma) with the youngest magmatic ages late Neoproterozoic-Early Cambrian, Triassic (240 Ma), and Eocene (48 Ma). εHf (t) values for zircon grains range from −23.95 to 13.13 for biotite granites (Type 1), −4.76 to 6.78 for amphibolites, and − 6.25 to 6.96 for Eocene mafic-felsic rock units. Biotite granites (Type 1) have I&lt;sub&gt;Sr&lt;/sub&gt; and εNd values ranging from 0.7177 to 0.7308 and − 14.8 to −7.4, respectively, whereas these values for the amphibolites are 0.7056 to 0.7090 and − 4.4 to 11.3, respectively. The mid-Eocene rock units of the CCC have I&lt;sub&gt;Sr&lt;/sub&gt; of 0.7050 to 0.7136 and εNd values of −3.9 to 8.9 gabbro-diorite-granodiorite, 3.3 to 16.3 for quartz diorite, and − 5.3 to −0.9 biotite granite (Type 2). The recorded zircon Hf isotopes along with I&lt;sub&gt;Sr&lt;/sub&gt; and εNd values indicate that a hybrid and old mantle (MORB+OIB) previously metasomatised by subduction of old enriched components (biotite granite Type 1) into the mantle, predating Eocene appinite-like mafic magma generation. Subsequent partial melts of such a source generate Eocene appinite magmas, as transitional rocks, which evolved to Eocene intermediate-felsic rocks through magma-crust interaction and accumulation/fractionation after the initial melts formed in the lower crust. The timing of the CCC formation (50–40 Ma) corresponds to an amphibolite metamorphism involving temperatures of 600–800 °C, associated with partial melting during the regional back-arc extension. The formation of new crust, through the reactivation and recycl","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126290"},"PeriodicalIF":2.6,"publicationDate":"2025-04-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143877471","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Spectroscopic signatures for expeditious monitoring of contamination risks at abandoned coal mine sites 用于快速监测废弃煤矿污染风险的光谱特征
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-04-11 DOI: 10.1016/j.chemer.2025.126292
Jelena Milinovic , Patrícia Santos , Jorge Espinha Marques , Deolinda Flores , Aurora Futuro , Carlos M. Pereira , Manuel Azenha
{"title":"Spectroscopic signatures for expeditious monitoring of contamination risks at abandoned coal mine sites","authors":"Jelena Milinovic ,&nbsp;Patrícia Santos ,&nbsp;Jorge Espinha Marques ,&nbsp;Deolinda Flores ,&nbsp;Aurora Futuro ,&nbsp;Carlos M. Pereira ,&nbsp;Manuel Azenha","doi":"10.1016/j.chemer.2025.126292","DOIUrl":"10.1016/j.chemer.2025.126292","url":null,"abstract":"<div><div>Soil acts as a natural ‘filter’, playing a crucial role in the transfer of geogenic and anthropogenic pollutants from abandoned coal mine sites to surrounding water bodies. Key indicators of soil contamination, such as pH, electrical conductivity (EC), and organic matter (OM), expressed as loss-on-ignition (LOI), can signal contamination risks when they deviate from optimal ranges. To enable sustainable risk assessment through monitoring of pH, EC, and LOI, streamlined spectroscopic techniques Fourier transform infrared (FTIR), near-infrared (NIR), Raman, and X-ray fluorescence (XRF) were applied in combination with multivariate analysis (MVA), to soil samples from two abandoned coal mines in NW Portugal. Partial least squares (PLS) regression models demonstrated that XRF spectroscopic data provided the most accurate assessment of soil pH, EC, and LOI at the local scale (R<sup>2</sup> = 0.92–0.99). The most significant spectroscopic signatures, identified through weighted regression coefficients (B<sub>w</sub>), enabled robust predictions of these key soil parameters. These findings highlight that these geochemical variables outperform molecular spectroscopy techniques for efficient and environmentally relevant risk monitoring of contamination in abandoned coal mine sites.</div></div>","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126292"},"PeriodicalIF":2.6,"publicationDate":"2025-04-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143828522","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Melting experiments of an L6 ordinary chondrite: Implications for the formation of alkali-rich achondrites L6普通球粒陨石的熔化实验:对富碱球粒陨石形成的启示
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-04-10 DOI: 10.1016/j.chemer.2025.126293
S. Iannini Lelarge , M. Masotta , L. Folco , T. Ubide , M.D. Suttle , L. Pittarello
{"title":"Melting experiments of an L6 ordinary chondrite: Implications for the formation of alkali-rich achondrites","authors":"S. Iannini Lelarge ,&nbsp;M. Masotta ,&nbsp;L. Folco ,&nbsp;T. Ubide ,&nbsp;M.D. Suttle ,&nbsp;L. Pittarello","doi":"10.1016/j.chemer.2025.126293","DOIUrl":"10.1016/j.chemer.2025.126293","url":null,"abstract":"<div><div>We conducted high-pressure (1 GPa) melting experiments (1100–1400 °C) on the equilibrated ordinary chondrite DAV 01001 (L6) to investigate partial melting scenarios of planetary embryo in the early solar system. At 1100 °C, no melting of the silicate phase is observed, and the initial chondritic texture is preserved, but the metallic-sulphidic phases formed two immiscible Fe–Ni and S-rich liquids. Melting of silicate minerals began at 1200 °C, progressing from plagioclase to high-Ca and low-Ca pyroxene and olivine. As melting advanced, the formation of new olivine and low-Ca pyroxene resulted in the production of trachy-andesitic melt at 1200 °C, basaltic trachy-andesitic melt at 1300 °C, and andesitic melt at 1400 °C. These silicate melts have chemical similarities with some anomalous achondrites (e.g., GRA 60128/9). At the same time, minerals of new formation resemble those of primitive achondrites (e.g., brachinites, ureilites, IAB silicate inclusions, acapulcoites and lodranites). The rapid mineral-liquid re-equilibration suggests that basaltic liquids can form only above 1400 °C and that relatively high degrees of melting (&gt;20 %) and crystallisation are necessary to explain the observed diversity of achondritic lithologies. These findings suggest that partial melting and recrystallization processes within planetary embryos could have played a critical role in the early solar system, contributing to the early differentiation of planetary bodies and the diversity of achondritic lithologies, including (but not limited to) alkali-rich achondrites.</div></div>","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126293"},"PeriodicalIF":2.6,"publicationDate":"2025-04-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143873763","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Deciphering the magmatic evolution of the Hyblean Cretaceous volcanism (SE Sicily, Italy): New geochemical, isotopic and noble gas analyses 意大利西西里岛东南部Hyblean白垩纪火山活动岩浆演化:新的地球化学、同位素和稀有气体分析
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-04-05 DOI: 10.1016/j.chemer.2025.126289
M. Di Bella , D. Romano , V. Volpi , F. Italiano , A. Correale , M. Petrelli , G. De Rosa , A. Tripodo , G. Sabatino
{"title":"Deciphering the magmatic evolution of the Hyblean Cretaceous volcanism (SE Sicily, Italy): New geochemical, isotopic and noble gas analyses","authors":"M. Di Bella ,&nbsp;D. Romano ,&nbsp;V. Volpi ,&nbsp;F. Italiano ,&nbsp;A. Correale ,&nbsp;M. Petrelli ,&nbsp;G. De Rosa ,&nbsp;A. Tripodo ,&nbsp;G. Sabatino","doi":"10.1016/j.chemer.2025.126289","DOIUrl":"10.1016/j.chemer.2025.126289","url":null,"abstract":"<div><div>The coupling of helium isotopes in fluid inclusions with conventional geochemical data provided a new perspective on the volcanic processes that took place during the Cretaceous in southern Sicily. Our new investigations reveal that during two distinct volcanic phases in the Late Cretaceous, magmas formed from low degrees of partial melting of a heterogeneous mantle source characterized by spinel lherzolite and varying garnet content. The collected samples, including lava flows, dikes, and sills, exhibit a wide range of rock types, from picritic basalts to hawaiites. Two different magma types were identified: one displaying a bell-shaped pattern akin to ocean island basalts (OIB) and another with an irregular pattern marked by positive spikes in Nb, K, Pb, Sr, Zr, and Ti. Strontium and Neodymium isotope compositions are weakly radiogenic, while the Pb isotope systematics show strong radiogenic values (<sup>206</sup>Pb/<sup>204</sup>Pb = 19.64–20.42; <sup>207</sup>Pb/<sup>204</sup>Pb = 15.61–15.70; <sup>208</sup>Pb/<sup>204</sup> Pb = 39.26–39.98), corresponding to the mantle focal zone (FOZO) component. The observed <sup>3</sup>He/<sup>4</sup>He ratios of 3.48 to 6.48 R<sub>c</sub>/R<sub>a</sub> in pyroxene fluid inclusions reflect the occurrence of pre-eruptive processes such as diffusion-induced fractionation or diffusive exchange taking place during magma residence in the crust. The <sup>3</sup>He/<sup>4</sup>He ratios from 7.75 to 9.31 R<sub>c</sub>/R<sub>a</sub> in olivine crystals are typical of MORB-type basalts, and they likely represent the original signature of the mantle source. The olivine R<sub>c</sub>/R<sub>a</sub> values may indicate an interaction with recycled (U+Th)-poor lithologies or high <sup>3</sup>He/<sup>4</sup>He materials in the upper mantle source. Furthermore, the <sup>3</sup>He/<sup>4</sup>He isotope ratios of olivines differ from those determined in the same region for Plio-Pleistocene volcanic products, for which a common origin has been suggested in the majority of previous studies. In light of our findings, the hypothesis that the Hyblean Late Cretaceous and Plio-Pleistocene volcanics are part of a single magmatic suite should be reexamined. Overall, our results indicate that the evolution of those volcanic rocks was influenced by fractional crystallization and accumulation processes providing additional details on the mantle source that may have been overlooked in the past.</div></div>","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126289"},"PeriodicalIF":2.6,"publicationDate":"2025-04-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143808325","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The petrology and geochemistry of the Montagna Grande-Monte Gibele trachytic shield volcano (Pantelleria, Italy) Montagna Grande-Monte Gibele粗质盾状火山(Pantelleria)的岩石学和地球化学
IF 2.6 3区 地球科学
Chemie Der Erde-Geochemistry Pub Date : 2025-04-01 DOI: 10.1016/j.chemer.2025.126288
John C. White , Ray Macdonald , Pierangelo Romano , Bogusław Bagiński , Silvio G. Rotolo , Beata Marciniak-Maliszewska , Alessandra Cinquegrani
{"title":"The petrology and geochemistry of the Montagna Grande-Monte Gibele trachytic shield volcano (Pantelleria, Italy)","authors":"John C. White ,&nbsp;Ray Macdonald ,&nbsp;Pierangelo Romano ,&nbsp;Bogusław Bagiński ,&nbsp;Silvio G. Rotolo ,&nbsp;Beata Marciniak-Maliszewska ,&nbsp;Alessandra Cinquegrani","doi":"10.1016/j.chemer.2025.126288","DOIUrl":"10.1016/j.chemer.2025.126288","url":null,"abstract":"<div><div>The 45.7 ± 1.0 ka (2σ) eruption of the compositionally zoned (comenditic trachyte to pantellerite) Green Tuff ignimbrite on the volcanic island of Pantelleria, Italy, was followed by the extrusion of a series of post-caldera metaluminous to mildly peralkaline trachyte lavas between 26.2 ± 2.0 and 22.3 ± 2.9 ka (2σ). This study uses whole-rock major- and trace-element compositions, mineral compositions, geothermobarometry, and petrogenetic models to examine the role of trachytes in the evolution of the Pantelleria magma system. Although previous studies have suggested that all of these units are consanguineous and form a liquid line of descent (LLOD) from metaluminous trachyte to peralkaline trachyte and pantellerite, mineralogical and geochemical evidence, as well as the results of modelling, suggest a much more complex origin. The crystallization of alkali feldspar from metaluminous trachyte liquids (descended from alkali to transitional basaltic magma <em>via</em> fractional crystallization) drives the composition of the residual melt to increasingly peralkaline compositions: pantelleritc trachyte first and then, after &gt;65 % crystallization, to pantellerite. This also results in the formation of a syenitic cumulate. Later intrusion of new mafic melt into the cumulate initiates partial melting, which produces comenditic trachyte melts characterized by low concentrations of incompatible trace elements (Rb, Zr, Nb, Th), high concentrations of Ba and Sr, and strong positive Eu anomalies. Entrainment of trachytic alkali feldspars into these melts as antecrysts further enhances these characteristics in whole-rock compositions. The origin of compositional zoning in the Green Tuff can be attributed to fractional crystallization from metaluminous trachyte within the lower pantelleritic portion and to partial melting of the syenitic cumulate for the upper comenditic trachyte portion.</div></div>","PeriodicalId":55973,"journal":{"name":"Chemie Der Erde-Geochemistry","volume":"85 3","pages":"Article 126288"},"PeriodicalIF":2.6,"publicationDate":"2025-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143776468","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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