Geochemical Characteristics of A-Type Granite near the Hongyan Cu-Polymetallic Deposit in the Eastern Hegenshan-Heihe Suture Zone, NE China: Implications for Petrogenesis, Mineralization and Tectonic Setting

Chen, Mao; Lü, Xinbiao; Chen, Chao

doi:10.3390/min9050309

Cited by 7 publications

(5 citation statements)

References 99 publications

(184 reference statements)

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“…Dall'Agnol et al, 2012;Eby, 1990;Frost et al, 2001;Frost & Frost, 2011;Whalen et al, 1987). These granitoids, which are bimodally associated with (voluminous) gabbro and/or basaltic rocks (Whalen & Currie, 1984;Clemens et al, 1986;also Yoder, 1973 and references therein), have received much attention among geologists for their economic potential and tectonic significance (e.g., Mao et al, 2019;Whalen et al, 1987 and references therein). Although A-type granitoids have an important role in the stabilization of the Archaean continental crusts, the origin of this group of granitoid rocks is debatable (e.g., Bailey, 1974;Barker et al, 1975;Bonin, 1998Bonin, , 2007Collins et al, 1982;Creaser et al, 1991;Cullers et al, 1981;Eby, 1990;Loiselle & Wones, 1979;Martin, 2006;Pitcher, 1983;Rajesh, 2000;Sheraton & Black, 1988;Skjerlie & Johnston, 1993;Turner et al, 1992;Whalen et al, 1987).…”

Section: Introductionmentioning

confidence: 99%

Geochemical evolution of the Lebowa Granite Pluton in western Bushveld Igneous Complex, South Africa: More insight into the evolution of bimodal A‐type granitoid

Mutele

Misra

2021

Geological Journal

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The 2.05 Ga Bushveld Igneous Complex (BIC) in the Kaapvaal Craton, South Africa, with an areal extent of 65,000 km 2 , represents one of the largest bimodal A-type granitoid suites in the world. The igneous activity of this complex begun with the Rooiberg Group of basalt-rhyolite bimodal volcanism, followed by the emplacement of the ultramafic-mafic Rustenburg Layered Suite (RLS), and finally the granitoid rocks of the Rashoop Granophyre (RG) and Lebowa Granite Suite (LGS). In this study, we present our new borehole description and whole-rock chemical data on the LGS from the relatively unknown western BIC to constrain the origin of the LGS and try to evaluate their geochemical relationship to the Rooiberg Group felsic volcanics. In the western BIC, the LGS is locally represented by the hydrothermally altered Paalkraal Granite and the Kenkelbos Granite that together form a central dome-like feature. The Veekraal Granite forms the peripheral part of the dome. These granitoids are, in general, coarse-grained, porphyritic, or equigranular, showing granophyric intergrowth, and consist of quartz, perthitic microcline, and albitic plagioclase with minor opaque and interstitial hornblende/biotite. Our whole-rock chemical data on western LGS, along with those from the Groblersdal area, eastern BIC (taken as reference), form a cluster in the 'granite' field in the normative Ab-An-Or diagram with mean Or/(Ab+Or) 0.5 (0.11), and are peralkaline to weakly peraluminous in composition. These A-type granitoids are strictly 'ferroan' and calc-alkalic to alkali-calcic in nature, and evolved through partial melting as evident mainly in process identification plots. In bulk chemical composition, the LGS and high-SiO 2 Rooiberg Group rhyolites overlap with the experimental melts generated during dehydration melting of tonalite-granodiorite, indicating the Archaean Kaapvaal TTG as their possible source.Constraints from experimental petrology further suggest the pressure and temperature of this relatively anhydrous (≤1 wt% H 2 O) melting were 2-1 kbar (i.e., ≤7.5 km crustal depth) and 920 C, respectively. As suggested before, the parent magma of the voluminous mafic-ultramafic body (RLS) of the BIC, forming a voluminous magma chamber in shallow crustal depth, provided the heat for this partial melting event.The following igneous event as evident from field description in the literature, our new borehole description and whole-rock chemical data, were a limited chemical

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Section: Introductionmentioning

confidence: 99%

Geochemical evolution of the Lebowa Granite Pluton in western Bushveld Igneous Complex, South Africa: More insight into the evolution of bimodal A‐type granitoid

Mutele

Misra

2021

Geological Journal

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“…Сокращения (а): континентальные массивы (супертеррейны): АР -Аргунский, БЦ -Бурея-Цзямусинский в составе: Буреинского (БЦ(Б)), Малохинганского (БЦ(М)), Ханкайского (БЦ(Х)), складчатые пояса: МО -Монголо-Охотский, СЛ -Солонкерский, ЮМ -Южно-Монгольско-Хинганский (НСТ -Нора-Сухотинский террейн). На врезке (б) показано положение исследуемых образований Нора-Сухотинского террейна, по [4], а также сутурных зон, по [24,28,33,38,39]: 1 -Муданьцзян (Mudanjiang); 2 -Дуньхуа-Мишань (Dunhua-Mishan); 3 -Цзямуси-Ютонг (Jiamusi-Yitong); 4 -Солонкер-Хра Морон-Чанчунь (Solonker-Xra Moron-Changchun); 5 -Хэгэншань-Хэйхэ (Hegenshan-Heihe) 6 -Хигуита-Тайюань (Xiguitu-Tayuan). а -раннепермские гранитоиды массива Шаншенфу (Shanshenfu) Хэгэншань-Хэйхэ сутурной зоны [28], б -раннепермские вулканиты массива Сонджен-Чжангуанцай (Songnen-Zhangguangcai) [22], в -раннепермские сиенограниты массива Синъян (Xing'an) [33], г -раннепермские гранитоиды массива Синъян (Xing'an) [20], д -раннепермские щелочные граниты массива Дахейшань (Daheishan) Хэгэншань-Хэйхэ сутурной зоны [37].…”

unclassified

“…Согласно геофизическим исследованиям [15], коллизия блоков Синъян (Xing'an) и Сонджен (Songnen), закрытие палеоокеана и формирование ХХСЗ происходили начиная с ~320 млн лет до ~290 млн лет назад. Кроме того постколлизионный этап ХХСЗ охарактеризован массивами гранитоидов А-типа с возрастом 292 ± 4 млн лет, 299 ± 1 и 298 ± 1 млн лет [28,37], сформированных в результате отрыва слэба (slab break-off ).…”

unclassified

“…Nd/144 Nd соответствуют последним значащим цифрам после запятой.Условные обозначения: 1 -позднекаменноугольные риолиты Приамурского фрагмента Нора-Сухотинского террейна, 2 -раннепермские гранитоиды массива Шаншенфу (Shanshenfu) ХХСЗ[28], 3 -раннепермские щелочные граниты массива Дахейшань (Daheishan) ХХСЗ[37]. Сокращения (в): A -гранитоиды А-типа, OGT -нефракционированные гранитоиды M-, I-и S-типов; FG -фракционированные гранитоиды; FeO* -суммарное железо в форме FeO.…”

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Late Carboniferous Rhyolites of the Amur Fragment of the Nora-Sukhotino Terrane: Geochemistry and Geochronology

Smirnov,

Khubanov,

Dril’

2023

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The publication presents the first results of geochemical, isotope-geochemical (Sm-Nd) and geochronological (U-Pb, LA-ICP-MS) studies on acid volcanic rocks collected in the Bogdanikha River basin of the Amur fragment of the Nora-Sukhotino terrane in the northeast of the South Mongoli–Khingan orogenic belt. In terms of the content of rock-forming components, the studied volcanic rocks correspond to high-silica and high-alumina rhyolites. Elevated contents of alkalis, Ga, Zr, Nb and Y, reduced concentrations of Ba, Sr, Ti, Eu, and mantle values of εNd(t) = +3.0…+3.6 enable the rhyolites from the Bogdanikha river basin to be classified as A2-type rhyolites. The concordant age of the youngest zircon population from the rhyolite, according to geochronological (U-Pb, LA-ICP-MS) studies, is 301  4 Ma which corresponds to the Late Carboniferous. Taking into account the geochemical features of the studied rhyolites and the existing models for the formation of the South Mongolian–Khingan orogenic belt, it is most likely that they formed in a collisional setting as a result of slab detachment.

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“…In addition, garnet Sm-Nd dating is conducted on the Hongshan skarn deposits to further constrain the timing of skarn formation in Zu et al [27]. The emplacement ages and geochemical and isotopic signatures of ore-related intrusions are also proved to be genetically linked with the formation of mineral deposits [28][29][30][31][32][33][34].…”

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confidence: 99%

Editorial for Special Issue “Polymetallic Metallogenic System”

Yang

2019

Minerals

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In the last century, following the development of Earth System Science, the metallogenic system has become an important topic in the study of mineral deposits. The term "metallogenic system" firstly presented in 1970s, connotes a natural system with ore-forming functions [1]. The metallogenic system includes geological factors controlling ore-formation and preservation, and ore-forming processes and their products-ore deposit series and anomaly series [1]. It emphasizes the integration of tectonic settings, controlling factors, metallogenic mechanisms, and conditions and mechanisms of post-mineralization transformation and preservation (i.e., the source, transport, trap, transformation, and preservation). On the basis of the theory of the metallogenic system, Deng et al. [2][3][4] defined the composite metallogenic system and summarized the distribution and characteristics of composite metallogenic systems in China.While economic geology typically focuses on the differences between individual deposits, the metallogenic system looks for broad similarities in each system [5]. The metallogenic system model allows for multiple mineralization styles to be identified within a single system [5]. For example, a porphyry copper system may develop associated high and low sulfidation epithermal gold mineralization, and skarn-type or hydrothermal vein-type Cu-Pb-Zn-Ag mineralization [6][7][8]. By integrating all geological ingredients and processes that are necessary for the formation of mineral deposits, the investigation of the metallogenic system is more useful for revealing the geodynamic evolution of a region, and more effective for regional prospecting exploration [9][10][11] From the perspective of regional metallogeny, the study by Niu et al. [12] relates deep dynamic processes in the Earth to gold deposits at the crustal surface (core → mantle → crust) in Jiaodong Province. Zircon Hf and whole-rock Nd isotopic mapping presented in Zhang et al. [13] precisely illustrate the controls of lithospheric architecture on the distribution of regional polymetallic mineralization. Liu et al. [14] and Wei et al. [15] propose the main gold deposition mechanisms by studying the fluid inclusions and corresponding H-O-S isotopic compositions of different ore-forming stages in the Sanshandao and Sizhuang gold deposits, respectively. Zhao et al. [16] classifies the Koka gold deposit in NE Africa as an orogenic gold deposit based on the similar features of geology and ore-forming fluids.The study by Chen et al. [17] describes the occurrence of texturally heterogeneous gold-hosting quartz types and variations in trace element geochemistry, offering a more multi-generational perspective on precipitation mechanisms that fluid inclusion studies may not be able to offer. Guo et al. [18] investigates the rare earth element geochemistry and C-O isotope characteristics of hydrothermal calcites to provide new insights into the fluid-rock interactions and ore-forming processes. Li N. et al. [19] present a textural and trace-element analysi...

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Geochemical Characteristics of A-Type Granite near the Hongyan Cu-Polymetallic Deposit in the Eastern Hegenshan-Heihe Suture Zone, NE China: Implications for Petrogenesis, Mineralization and Tectonic Setting

Cited by 7 publications

References 99 publications

Geochemical evolution of the Lebowa Granite Pluton in western Bushveld Igneous Complex, South Africa: More insight into the evolution of bimodal A‐type granitoid

Geochemical evolution of the Lebowa Granite Pluton in western Bushveld Igneous Complex, South Africa: More insight into the evolution of bimodal A‐type granitoid

Late Carboniferous Rhyolites of the Amur Fragment of the Nora-Sukhotino Terrane: Geochemistry and Geochronology

Editorial for Special Issue “Polymetallic Metallogenic System”

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