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Zircon Coupled Dissolution–Precipitation Replacement During Melt–Rock Interaction Modifies Chemical Signatures Resulting in Misleading Ages 熔岩-岩石相互作用过程中的锆石耦合溶解-沉淀置换改变了化学特征,导致误导年龄
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-10-15 DOI: 10.1111/jmg.12796
Nathan R. Daczko, Victoria Elliott, Sandra Piazolo, Kevin Hao

Melt migration through Earth's crust drives well-documented melt–rock reactions, locally changing rock assemblage and geochemistry. However, melt–zircon interaction remains understudied. We report on three zircon-melt interaction events from the Pembroke Granulite, New Zealand. Primary zircon from gabbroic gneiss which was subject to minor post-emplacement melt migration and primary zircon from younger dykes exhibit straightforward microstructures, microchemistry, and age data. In contrast, zircon from melt-mediated reaction halos adjacent to the dykes and from melt-fluxed high-strain zones display dissolution modification of grains, micro-porosity and blurred or truncated internal zoning typical of replacement by coupled dissolution-precipitation. Replaced zircon domains show changed rare earth element patterns and redistributed or lost radiogenic Pb that generates ambiguous apparent spot date arrays, smeared over tens of millions of years. We conclude that the metamorphism and three melt–rock interaction events were brief, and the arrays misrepresent the true age and duration of the metamorphism. Pb-loss persisted beyond the metamorphism, with porosity and inclusions formed during coupled dissolution-precipitation making replaced zircon domains more susceptible to subsequent Pb-loss compared to the structurally intact, primary magmatic zircon in the host gabbroic gneiss or dykes. We recommend conducting high-resolution microstructural investigations upon recognition of spot date arrays observed in single samples to rule out the possibility of spurious arrays resulting from coupled dissolution-precipitation.

熔体在地壳中的迁移推动了有据可查的熔岩反应,局部改变了岩石组合和地球化学。然而,对熔体-锆石相互作用的研究仍然不足。我们报告了新西兰彭布罗克花岗岩中的三个锆石-熔体相互作用事件。来自辉长岩片麻岩的原生锆石和来自较年轻岩堤的原生锆石在置换后发生了轻微的熔融迁移,显示出简单明了的微结构、微化学和年龄数据。与此相反,来自堤坝附近熔融介导的反应晕和熔融流出的高应变区的锆石则显示出晶粒的溶解改性、微孔和模糊或截断的内部分带,这是典型的溶解-沉淀耦合置换现象。被置换的锆石域显示出稀土元素模式的改变,以及放射性铅的重新分布或丢失,从而产生了模糊的表观点日期阵列,时间跨度达数千万年。我们的结论是,变质作用和三次熔岩相互作用事件都很短暂,这些阵列错误地反映了变质作用的真实年龄和持续时间。铅流失在变质作用之后依然存在,由于在溶解-沉淀耦合过程中形成的多孔性和包裹体,与主辉长岩片麻岩或岩堤中结构完整的原生岩浆锆石相比,被取代的锆石域更容易受到后续铅流失的影响。我们建议在确认单个样品中观察到的点状日期阵列后,进行高分辨率的微结构调查,以排除耦合溶解-沉淀作用产生的虚假阵列的可能性。
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引用次数: 0
Pressure–Temperature–Time Evolution of a Polymetamorphic Paragneiss With Pseudomorphs After Jadeite From the HP–UHP Gneiss-Eclogite Unit of the Variscan Erzgebirge Crystalline Complex, Germany 德国瓦里斯坎-埃尔茨盖比尔格结晶复合体 HP-UHP Gneiss-Eclogite 单元中具有翡翠后假形态的多变质副辉石的压力-温度-时间演化
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-09-17 DOI: 10.1111/jmg.12794
Hans-Joachim Massonne

A quartz-rich paragneiss from the Variscan Erzgebirge Crystalline Complex (ECC) was studied in detail because of abundant millimetre-sized and clearly oriented pseudomorphs after a sodic mineral interpreted to have been jadeite. This mineral, or pseudomorphs after it, is rarely found in extensive high-pressure (HP)–ultrahigh-pressure (UHP) terranes worldwide despite reported pressure–temperature (P–T) conditions suitable for the formation of jadeite in common paragneisses and orthogneisses. In the studied rock, which contains abundant large and oriented potassic white mica flakes and minor millimetre-sized garnet grains, the pseudomorphs consist of clusters of small albite grains with thin phengitic muscovite flakes in between. X-ray maps for Ca and Mg in garnet demonstrate that an early generation of this mineral (Gt1) was corroded and subsequently overgrown by a Ca-richer generation (Gt2). White mica is phengite with maximum Si contents of 3.42 atoms per formula unit. P–T conditions of 0.85 GPa and 650°C and 1.7 GPa and 660°C were derived for the formation of Gt1 and Gt2 rim + Si-rich phengite, respectively, using pseudosection modelling. The latter conditions representing the pressure peak experienced by the paragneiss are compatible with the original presence of jadeite and possibly paragonite as well. This metamorphic peak occurred at 338.4 ± 2.3 (2σ) Ma based on in situ dating of monazite grains with the electron microprobe. A single monazite age of 386.4 ± 10.5 (2σ) Ma is related to the formation of Gt1. Thus, a Late Devonian metamorphism is suggested here for the first time to have occurred in ECC gneisses before the major HP event in the Early Carboniferous. Furthermore, the study demonstrates that the eclogite-facies gneisses of the Gneiss-Eclogite Unit of the ECC experienced peak pressures of not more than 2 GPa in contrast to recent proposals of an extensive UHP area in this unit. In addition, it is suggested that the localized occurrence of UHP rocks surrounded by other lithologies otherwise lacking evidence for UHP conditions should be interpreted with caution with respect to their regional extent and significance.

我们对瓦里斯坦时代埃尔茨盖比尔格结晶群(ECC)中的一种富含石英的片麻岩进行了详细研究,因为其中有大量毫米大小、取向清晰的假象,而这种假象被解释为翡翠的钠长石矿物。尽管有报道称在普通片麻岩和正长片麻岩中存在适合翡翠形成的压力-温度(P-T)条件,但在全球广泛的高压(HP)-超高压(UHP)地层中很少发现这种矿物或其假象。在所研究的岩石中,含有丰富的大型定向钾长石白云母片和少量毫米大小的石榴石颗粒,假象由小白云母颗粒群组成,中间夹着薄薄的黝帘石片。石榴石中钙和镁的 X 射线图显示,这种矿物的早期一代(Gt1)被腐蚀,随后被钙富集的一代(Gt2)所覆盖。白云母是辉绿岩,每式单位的最大硅含量为 3.42 个原子。利用假吸力建模法推导出 Gt1 和 Gt2 边缘+富硅辉绿岩形成的 P-T 条件分别为 0.85 GPa 和 650°C 以及 1.7 GPa 和 660°C。后一种条件代表了辉绿岩所经历的压力峰值,与原来存在的翡翠以及可能存在的副皂石相吻合。根据电子显微镜对独居石晶粒的现场测年,变质峰值出现在 338.4 ± 2.3 (2σ) Ma。Gt1 的形成与 386.4 ± 10.5 (2σ) Ma 的单一独居石年龄有关。因此,这里首次提出了晚泥盆世变质作用发生在早石炭世主要HP事件之前的ECC片麻岩中。此外,该研究还表明,ECC片麻岩-蚀变片麻岩单元的蚀变片麻岩经历的峰值压力不超过2 GPa,这与最近关于该单元存在大面积超高压区的建议形成了鲜明对比。此外,研究人员还建议,对于局部出现的超高压岩石,以及周围缺乏超高压条件证据的其他岩性,在解释其区域范围和意义时应谨慎从事。
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引用次数: 0
Experimental Replacement of Zircon by Melt-Mediated Coupled Dissolution-Precipitation Causes Dispersion in U–Pb Ages 熔融介导的溶解-沉淀耦合实验置换锆石导致 U-Pb 年代的分散
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-08-27 DOI: 10.1111/jmg.12795
Jeremy L. Asimus, Nathan R. Daczko, Jean-Antoine Gazi, Isra S. Ezad, Ivan Belousov, Thomas Rodemann, Jacqueline A. Halpin, Sandra Piazolo

Zircon geochronology provides critical information on the rates and durations of geological processes and enables researchers to explore deep time. However, some zircon datasets show a continuum of concordant ages (‘smear’) without well-defined age populations. These age smears are typically interpreted to represent variable loss of radiogenic Pb or protracted geological events lasting tens of millions of years. Coupled dissolution-precipitation replacement of zircon has been suggested as one process that may produce these complex age datasets. Here, we react fragments of the well characterised Mud Tank zircon standard with natural intermediate and mafic melts (0.9 GPa, 1100–1180°C) to test if short-term exposure to a melt can modify the geochronological patterns of zircon. Our observations show that within a short duration (18 h to 3.5 days), most Mud Tank zircon fragments display microstructural and/or chemical evidence for modification by dissolution at fragment boundaries along with partial replacement by coupled dissolution-precipitation processes. The replaced zircon domains have U–Pb ages that smear over one hundred million years, between 764–647 Ma, illustrating variable mobility and redistribution of the U and Pb isotopes. Our experiments demonstrate that zircon modified by coupled dissolution-precipitation replacement may not faithfully record the age or duration of geological events and that investigation of zircon microstructure in high-resolution backscattered electron, cathodoluminescence imaging and/or Raman mapping is needed to better understand complex zircon geochronological datasets.

锆石地质年代学提供了有关地质过程的速率和持续时间的重要信息,使研究人员能够探索深部时间。然而,一些锆石数据集显示出连续的一致年龄("涂抹"),而没有明确的年龄群。这些年龄斑点通常被解释为放射性铅的可变损失或持续数千万年的漫长地质事件。锆石的溶解-沉淀耦合置换被认为是产生这些复杂年龄数据集的一个过程。在这里,我们将特性良好的泥潭锆石标准碎片与天然的中间熔体和岩浆熔体(0.9 GPa, 1100-1180°C)进行反应,以测试短期暴露于熔体是否会改变锆石的地质年代模式。我们的观察结果表明,在短时间内(18 小时至 3.5 天),大多数泥罐锆石碎片显示出微观结构和/或化学证据,表明碎片边界处的溶解以及溶解-沉淀耦合过程的部分置换改变了锆石。被置换的锆石区域的 U-Pb 年龄在 1 亿年(764-647 Ma)之间,说明了 U 和 Pb 同位素的可变流动性和再分布。我们的实验表明,通过溶解-沉淀耦合置换改变的锆石可能无法忠实地记录地质事件的年龄或持续时间,因此需要通过高分辨率反向散射电子、阴极发光成像和/或拉曼绘图来研究锆石的微观结构,以便更好地理解复杂的锆石地质年代数据集。
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引用次数: 0
Kyanite and Cordierite-Andalusite occurrences in parts of Barrow's Staurolite zones – The effects of high ferric iron 巴罗部分黝帘石带的黝帘石和堇青石-安达卢西亚石矿点--高铁的影响
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-08-07 DOI: 10.1111/jmg.12792
Ben Harte
<p>George Barrow's maps (<b>1893</b>, <b>1912</b>) of the metamorphic zones named after him in the south-eastern Scottish Highlands, show a prominent staurolite zone running from the west of Glen Clova to the North Sea coast near Stonehaven in the east. Pelitic mica schists throughout this zone commonly show principal mineral assemblages of staurolite+biotite+garnet+muscovite +quartz (St + Bt + Grt), with sodic plagioclase, ilmenite and sometimes magnetite as common accessories; these schists have bulk compositions corresponding with those of common Dalradian metasediments. However, the mineral assemblages on the low- and high-grade margins of the staurolite zone show evidence of changes from west to east. Lower grade assemblages near Stonehaven include chloritoid+biotite, which has not been found further west in the classic ‘Barrovian’ sequence; whilst the higher grade assemblages near Stonehaven lack kyanite, which is widely seen further west. The Stonehaven area has been suggested to have under gone metamorphism at lower pressure <i>(P)</i> than the classic region of the ‘Glens’ inland to the west.</p><p>This paper describes the occurrence at middle grade in the broad staurolite zone, of unusual bulk rock compositions showing high ratios of Fe<sub>2</sub>O<sub>3</sub>/(Fe<sub>2</sub>O<sub>3</sub> + FeO) and MgO/(MgO + FeO) (abbreviated to M/FM). The high M/FM assemblages are distinct from those of the common St-Bt-Grt schists. The high ratios of ferric to ferrous iron are thought to result from original sedimentary protolith compositions, that led to metamorphism at relatively high conditions of oxygen fugacity (ƒo<sub>2</sub>), and resulted in the formation of haematite-bearing assemblages, rather than ones carrying accessory ilmenite and magnetite as in the common St + Bt + Grt rocks.</p><p>In the west (Glen Lethnot), the haematite-bearing pelites show the occurrence of kyanite at a distinctly lower grade than the common (haematite-free) pelites, and a transition from staurolite-biotite (St + Bt) through staurolite–kyanite-biotite (St + Ky + Bt) to kyanite-biotite (Ky-Bt) assemblages occurs with increasing abundance of haematite and higher bulk M/FM values. In all bulk compositions, the upgrade formation of kyanite may be associated with the movement of the St + Ky + Bt assemblage to lower M/FM bulk compositions with increasing temperature (<i>T</i>). The difference in the temperature of lowest-grade kyanite formation in haematite-rich schists, compared with that in common haematite-free schists may approach 50°C.</p><p>In the east (Stonehaven section), the haematite-bearing assemblages are much rarer than in Glen Lethnot, but those found so far are very distinctive in showing large porphyroblasts of probable cordierite (typically altered to chlorite and sericite). Occasional assemblages of andalusite-cordierite-biotite (And-Crd-Bt) also occur in the haematite-bearing rocks and confirm lower pressures of metamorphism near Stonehaven than tho
乔治-巴罗(George Barrow)绘制的苏格兰高地东南部以他的名字命名的变质岩带地图(1893 年、1912 年)显示,从格伦克洛瓦(Glen Clova)西部到东部斯通海文附近的北海沿岸有一个突出的白云母带。整个该区域的辉石云母片岩通常显示出辉绿岩+黑云母+石榴石+褐铁矿+石英(St + Bt + Grt)的主要矿物组合,阳起石斜长石、钛铁矿和磁铁矿有时是常见的附属矿物;这些片岩的体质成分与常见的达拉得安基岩的体质成分相同。不过,在白云母带的低品位和高品位边缘,矿物组合显示出从西向东变化的迹象。斯通黑文附近的低品位矿物组合包括绿泥石+橄榄石,这在典型的 "巴罗维 "序列的更西部地区是没有发现的;而斯通黑文附近的高品位矿物组合则缺乏在更西部地区广泛存在的闪长岩。本文描述了在宽广的白云石区出现的中等品位不寻常的大块岩石成分,这些成分显示出较高的Fe2O3/(Fe2O3 + FeO)和MgO/(MgO + FeO)比率(简称M/FM)。高M/FM组合与常见的St-Bt-Grt片岩截然不同。铁和亚铁的高比率被认为是原始沉积原岩成分造成的,这种成分导致了在相对较高的富氧(ƒo2)条件下的变质作用,并形成了含血铁矿的集合体,而不是像常见的 St + Bt + Grt 岩石那样,形成了含有附属钛铁矿和磁铁矿的集合体。在西部(Glen Lethnot),与普通(不含血门石)辉绿岩相比,含血门石的辉绿岩中出现了明显品位较低的闪长岩,并且随着血门石含量的增加和块体 M/FM 值的升高,出现了从白云石-黑云母(St + Bt)到白云石-闪长岩-黑云母(St + Ky + Bt)再到闪长岩-黑云母(Ky-Bt)集合体的转变。在所有块体成分中,随着温度(T)的升高,闪长岩的升级形成可能与 St + Ky + Bt 组合向较低 M/FM 块体成分的移动有关。在东部(斯通哈文段),含血门石的集合体比 Glen Lethnot 要稀少得多,但迄今为止发现的集合体都非常独特,显示出可能是堇青石的大型斑块(通常被绿泥石和绢云母蚀变为绿泥石)。含血门石的岩石中偶尔也会出现安山岩-堇青石-黑云母(And-Crd-Bt)的集合体,这证实了斯通黑文附近的变质压力比更西边的克洛瓦格兰、莱特霍特和埃斯克格兰的变质压力要低。
{"title":"Kyanite and Cordierite-Andalusite occurrences in parts of Barrow's Staurolite zones – The effects of high ferric iron","authors":"Ben Harte","doi":"10.1111/jmg.12792","DOIUrl":"10.1111/jmg.12792","url":null,"abstract":"&lt;p&gt;George Barrow's maps (&lt;b&gt;1893&lt;/b&gt;, &lt;b&gt;1912&lt;/b&gt;) of the metamorphic zones named after him in the south-eastern Scottish Highlands, show a prominent staurolite zone running from the west of Glen Clova to the North Sea coast near Stonehaven in the east. Pelitic mica schists throughout this zone commonly show principal mineral assemblages of staurolite+biotite+garnet+muscovite +quartz (St + Bt + Grt), with sodic plagioclase, ilmenite and sometimes magnetite as common accessories; these schists have bulk compositions corresponding with those of common Dalradian metasediments. However, the mineral assemblages on the low- and high-grade margins of the staurolite zone show evidence of changes from west to east. Lower grade assemblages near Stonehaven include chloritoid+biotite, which has not been found further west in the classic ‘Barrovian’ sequence; whilst the higher grade assemblages near Stonehaven lack kyanite, which is widely seen further west. The Stonehaven area has been suggested to have under gone metamorphism at lower pressure &lt;i&gt;(P)&lt;/i&gt; than the classic region of the ‘Glens’ inland to the west.&lt;/p&gt;&lt;p&gt;This paper describes the occurrence at middle grade in the broad staurolite zone, of unusual bulk rock compositions showing high ratios of Fe&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;3&lt;/sub&gt;/(Fe&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;3&lt;/sub&gt; + FeO) and MgO/(MgO + FeO) (abbreviated to M/FM). The high M/FM assemblages are distinct from those of the common St-Bt-Grt schists. The high ratios of ferric to ferrous iron are thought to result from original sedimentary protolith compositions, that led to metamorphism at relatively high conditions of oxygen fugacity (ƒo&lt;sub&gt;2&lt;/sub&gt;), and resulted in the formation of haematite-bearing assemblages, rather than ones carrying accessory ilmenite and magnetite as in the common St + Bt + Grt rocks.&lt;/p&gt;&lt;p&gt;In the west (Glen Lethnot), the haematite-bearing pelites show the occurrence of kyanite at a distinctly lower grade than the common (haematite-free) pelites, and a transition from staurolite-biotite (St + Bt) through staurolite–kyanite-biotite (St + Ky + Bt) to kyanite-biotite (Ky-Bt) assemblages occurs with increasing abundance of haematite and higher bulk M/FM values. In all bulk compositions, the upgrade formation of kyanite may be associated with the movement of the St + Ky + Bt assemblage to lower M/FM bulk compositions with increasing temperature (&lt;i&gt;T&lt;/i&gt;). The difference in the temperature of lowest-grade kyanite formation in haematite-rich schists, compared with that in common haematite-free schists may approach 50°C.&lt;/p&gt;&lt;p&gt;In the east (Stonehaven section), the haematite-bearing assemblages are much rarer than in Glen Lethnot, but those found so far are very distinctive in showing large porphyroblasts of probable cordierite (typically altered to chlorite and sericite). Occasional assemblages of andalusite-cordierite-biotite (And-Crd-Bt) also occur in the haematite-bearing rocks and confirm lower pressures of metamorphism near Stonehaven than tho","PeriodicalId":16472,"journal":{"name":"Journal of Metamorphic Geology","volume":"42 8","pages":"1131-1158"},"PeriodicalIF":3.5,"publicationDate":"2024-08-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/jmg.12792","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141935193","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Probing intra-oceanic subduction infancy in ancient orogenic belts: Example from Chinese South Tianshan 古造山带洋内俯冲萌芽探测:以中国南天山为例
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-07-25 DOI: 10.1111/jmg.12793
Limin Gao, Wenjiao Xiao, Zhou Tan, Hao Cheng, Qigui Mao, Hao Wang, Xiaoliang Jia, Miao Sang, Yuhong Guo, Yiying Tan

Subduction infancy corresponds to the first few million years of the start of subduction following heat transfer from the incipient mantle wedge towards the slab-top, as witnessed by metamorphic soles which represent slivers of oceanic crust metamorphosed up to granulite facies conditions welded beneath obducted ophiolites. In this study, integrated petrological, geochemical, mineralogical, geochronological, and thermodynamic studies were carried out on samples from the Yushugou high-temperature metamorphic ophiolitic complex (YHTM) in the South Tianshan Accretionary Complex (STAC), where a massive exposure of coherent granulite accompanied by a thick peridotite body is preserved. Bulk-rock compositions and Sr–Nd–Hf isotopes demonstrate the petrogenesis of meta-basalts with oceanic island basalt (OIB)-like and mid-ocean ridge basalt (MORB)-like affinities, with little infiltration by subduction-derived melts and/or fluids (e.g., no negative Nb–Ta anomalies). Thermodynamic modelling and U–Pb chronology reveal that the YHTM meta-basalts experienced granulite facies metamorphism of ~840–940°C and ~0.92–1.02 GPa at c. 392 Ma and then possibly reheating and zircon alteration in the Carboniferous. In addition, detrital zircons in sedimentary host rocks of the YHTM show limited Precambrian records and offer maximum depositional ages of c. 410–400 Ma together with the oldest Palaeozoic cluster around c. 470–450 Ma. It is suggested that the YHTM granulites could be of Ordovician–Silurian protolith and such an age pattern significantly deviates from those of adjacent terranes (the Central Tianshan, STAC, and North Tarim Craton). Combined with the compilation of pressure–temperature–time estimates of the YHTM and ages of regional ophiolites, arc intermediate-mafic rocks, A-type granites, and deformation, a model of induced, temporarily northward, intra-oceanic subduction initiation is proposed, which probably occurred along the previously existing weak zone close to a seamount or oceanic plateau in the earliest middle Devonian during the northward subduction of the South Tianshan Ocean (STO). Anomalously high geothermal gradients could be triggered by asthenosphere upwellings, further facilitating the formation of OIB-type metamorphic soles. The YHTM, which represents the remnant of metamorphic soles and associated ophiolites, was finally emplaced to the north margin of the STAC during the relatively long-term (c. 160 million years) accretion and continuous subduction of the STO before its closure. This finding also presents a new natural example of OIB-type metamorphic soles as a snapshot of fossil intra-oceanic subduction infancy during the complex evolutionary history of the STO.

俯冲萌芽期相当于俯冲开始后的最初几百万年,热量从萌芽期的地幔楔向板顶传递,变质岩底就是证明,变质岩底代表了在俯冲蛇绿岩下焊接的变质为花岗岩面条件的洋壳薄片。在这项研究中,对来自南天山堆积复合体(STAC)榆树沟高温变质蛇绿岩复合体(YHTM)的样品进行了岩石学、地球化学、矿物学、地质年代学和热力学综合研究。块岩成分和 Sr-Nd-Hf 同位素表明,元玄武岩的成岩过程与大洋岛屿玄武岩(OIB)和大洋中脊玄武岩(MORB)相似,几乎没有来自俯冲的熔体和/或流体的渗透(例如,没有负 Nb-Ta 异常)。热力学模型和铀-铅年代学显示,YHTM元基性岩在大约392Ma时经历了大约840-940°C和大约0.92-1.02GPa的花岗岩变质作用,然后可能在石炭纪经历了再热和锆石蚀变作用。此外,豫东特提山脉沉积母岩中的锆英石显示出有限的前寒武纪记录,最大沉积年龄约为410-400 Ma,最古老的古生代群约为470-450 Ma。有研究认为,青藏高原花岗岩可能属于奥陶纪-志留纪原岩,这种年龄模式与邻近地块(中天山、STAC和北塔里木克拉通)的年龄模式明显不同。结合对YHTM的压力-温度-时间估算以及区域蛇绿岩、弧中岩、A型花岗岩和变形的年龄汇编,提出了一个诱导的、暂时向北的洋内俯冲起始模型,它可能发生在早泥盆世中期南天山洋向北俯冲的过程中,沿着先前存在的靠近海山或大洋高原的薄弱带发生。异常高的地热梯度可能是由星体层上涌引发的,从而进一步促进了OIB型变质岩溶的形成。YHTM代表了变质溶岩和相关蛇绿岩的残余,在STO关闭前相对长期(约1.6亿年)的增生和持续俯冲过程中,YHTM最终位于STAC的北缘。这一发现也为OIB型变质溶岩提供了一个新的自然实例,是STO复杂演化历史中洋内俯冲雏形化石的一个缩影。
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引用次数: 0
Isochemical metamorphism origin of the newly discovered Baqing jadeitoid, eastern-central Tibet, China 中国西藏中东部新发现的巴青玉石的等化学变质起源
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-07-11 DOI: 10.1111/jmg.12790
Xin Jin, Donna L. Whitney, Yu-Xiu Zhang, Hannah J. Blatchford, Kai-Jun Zhang, Tatsuki Tsujimori, Yuan-Yuan Xiao, Hai-Yang Liu, Anette von der Handt, Li-Long Yan, Yao Liu, Lu Lu, Cong-Ying Li

The formation of most jadeitites and other jadeite-rich rocks (jadeitoids) during subduction is thought to occur by precipitation (P-type) or metasomatism (R-type) by infiltration of Na-Al-Si-rich aqueous fluids because of the compositional similarity of the rocks to inferred subduction fluids. Whether these rocks can form by isochemical metamorphism (I-type) during subduction is still hotly debated. A characteristic of I-type jadeitoid is that it exhibits a similar prograde metamorphic record as associated eclogite, in contrast to P- and R-type jadeitite and jadeitoids that are typically enclosed in serpentinite derived from the mantle wedge and either lack a prograde metamorphic history (R-type and P-type) or probably experience a prograde history (R-type) that is difficult to discern owing to the high variance of the jadeite-dominated assemblages and alteration by subduction fluids. The recently discovered Baqing (eastern-central Tibet) jadeitoid is enclosed by quartzo-feldspathic schist and has a peak metamorphic assemblage of almandine + jadeite/omphacite + phengite/paragonite + rutile + quartz, similar to eclogite. Abundant mineral inclusions in almandine, especially rutile inclusions with increasing Zr contents from the core to rim of almandine, provide an opportunity to further decode the jadeitoid-forming processes. In this study, pseudosections and Zr-in-rutile thermometry, together with conventional geothermobarometers, were employed to decipher the metamorphic history of Baqing jadeitoids. Two analysed Baqing jadeitoids exhibit a similar clockwise PT path, starting from early metamorphic conditions of 5–7 kbar, 350–440°C, to different peak conditions (27–29 kbar, 730–760°C, or 20–23 kbar, 670–710°C), followed by relatively consistent retrograde metamorphic conditions of 6–7 kbar, 530–600°C. This result indicates a similar subduction history to the Baqing eclogite. In addition, the Baqing jadeitoids show similar geochemical characteristics to some Na-rich, K-depleted and Ca-depleted sedimentary rocks or plagiogranite. Therefore, we propose an isochemical genesis for the Baqing jadeitoid, rather than a metasomatic origin.

在俯冲过程中形成的大多数翡翠和其他富含翡翠的岩石(jadeitoids)被认为是通过富含Na-Al-Si的水性流体的渗透沉淀(P型)或变质作用(R型)形成的,因为这些岩石的成分与推断的俯冲流体相似。至于这些岩石是否会在俯冲过程中通过等化学变质作用(I型)形成,目前仍存在激烈的争论。I型硬玉的一个特点是与伴生的斜长岩具有相似的顺行变质记录,而P型和R型硬玉和硬玉通常被包裹在来自地幔楔的蛇纹岩中,要么缺乏顺行变质历史(R型和P型),要么很可能经历了顺行变质历史(R型),但由于硬玉为主的组合差异很大,加上俯冲流体的蚀变作用,很难辨别其顺行变质历史。最近发现的巴青(西藏中东部)类翡翠被石英-长石片岩所包围,其变质峰值组合为白云母+翡翠/闪长岩+辉石/霰石+金红石+石英,与埃克洛辉石相似。白云母中丰富的矿物包裹体,尤其是金红石包裹体,从白云母的核心到边缘,Zr含量不断增加,这为进一步解读翡翠的形成过程提供了机会。本研究采用假剖面和金红石中Zr含量热量测定法,以及传统的地温热压仪,对巴青玉石的变质历史进行了解密。所分析的两块巴青玉髓表现出相似的顺时针P-T路径,从5-7千巴、350-440摄氏度的早期变质条件,到不同的峰值条件(27-29千巴、730-760摄氏度,或20-23千巴、670-710摄氏度),然后是相对一致的6-7千巴、530-600摄氏度的逆变质条件。这一结果表明了与巴青斜长岩相似的俯冲历史。此外,巴青玉柱岩与一些富Na、贫K、贫C的沉积岩或斜长岩具有相似的地球化学特征。因此,我们提出了巴青翡翠的等化学成分成因,而非元古代成因。
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引用次数: 0
Hydration of mafic crustal rocks at high temperature during brittle-viscous deformation along a strike-slip plate boundary 沿走向-滑动板块边界的脆性-粘性变形过程中岩浆状地壳岩石在高温下的水合作用
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-07-10 DOI: 10.1111/jmg.12791
Laura Airaghi, Hugues Raimbourg, Tsuyoshi Toyoshima, Laurent Jolivet, Laurent Arbaret
<p>The Poroshiri ophiolite (Hidaka metamorphic belt, Japan) occurs within a crustal-scale network of high-temperature, dextral shear zones that accommodated hundreds of kilometres of displacement due to the opening of the Japan Sea in the Neogene. The opholitic rocks comprise ultramafic, mafic and sedimentary protoliths that have been variably hydrated and metamorphosed. This work investigates the mechanisms and timing of fluid influx relative to viscous deformation in metagabbros and amphibolites deformed during exhumation from granulite- to amphibolite-facies conditions. We consider a range of microstructures, from low strain domains and 1–2 mm thick shear bands to mylonites with a thickness of a few meters. Low strain domains of metagabbros exhibit corona textures with symplectites consisting of pargasitic amphibole (Ed<sub>0.7</sub>) - anorthitic plagioclase (An<sub>80–92</sub>) ± orthopyroxene ± clinopyroxene forming around olivine and igneous pyroxene and with similar plagioclase–amphibole-orthopyroxene ± clinopyroxene granoblastic aggregates in micrometric-thick fractures. These textures result from hydration under low fluid-rock ratio, with elevated H<sub>2</sub>O content only occurring locally (H<sub>2</sub>O > 1–1.2 wt%). Igneous mineral replacement leads to grain size reduction from 1 mm to ~10 μm. Amphibole exhibits a strong core-rim zonation primarily controlled by the high diffusivity of Fe, Mg and OH and the low diffusivity of Al. Mineral compositional equilibrium is achieved at the scale of 100–200 μm. In mm-thick localized shear bands and in metric-scale mylonitic amphibolites, the heterogeneous mineral composition of amphibole (Ed<sub>0.2–0.5</sub>) and plagioclase (An<sub>40−</sub>An<sub>80</sub>) indicates only partial re-equilibration (at the scale of 200–500 μm) despite higher fluid-rock ratios and more pervasive fluid percolation than in metagabbros. Plagioclase–amphibole thermometry and equilibrium phase diagrams indicate that the initial fluid infiltration and corona formation occurred at 800–850°C by fracturing and percolation along grain boundaries. This was followed by the main fluid percolation and mylonitization event, which occurred during exhumation and cooling at conditions of 720–580°C, ~4 kbar. Continuous hydration during retrogression was achieved by the influx of dominantly seawater-derived fluid, as attested by the high chlorine (Cl) contents (>300–400 ppm) of amphiboles in fractures. The heterogeneous distribution of fractures controls the distribution of fluid from the earliest stages of hydration, creating positive feedback where the growth of hydrous minerals as amphibole (up to +300 vol% of amphibole in high strain areas relative to the low-strain ones) and the formation of fine-grained mixed domains that led to further localization of viscous strain and mass transfer (variations of ± 30–40% in major elements). The Poroshiri ophiolite therefore represents a good fossil example of a former transpres
Poroshiri蛇绿岩(日本日高变质带)位于地壳规模的高温右旋剪切带网络内,由于新近纪日本海的开辟,该网络承受了数百公里的位移。鲕粒岩由超基性、基性和沉积原岩组成,经过不同程度的水化和变质作用。这项研究调查了在从花岗岩期向闪长岩期的剥蚀变形过程中,流体流入辉长岩和闪长岩的机制和时间,以及流体流入辉长岩和闪长岩与粘性变形的关系。我们考虑了一系列微结构,从低应变域和1-2毫米厚的剪切带到几米厚的岩浆岩。偏闪长岩的低应变域表现出电晕纹理,在橄榄石和火成辉石周围形成由副斜长石闪长石(Ed0.7)-正长石斜长石(An80-92)±正长石±霞石组成的共闪长岩,在微米厚的裂隙中形成类似的斜长石-闪长石-正长石±霞石的粒状集合体。这些纹理是在流体-岩石比值较低的情况下水化形成的,H2O 含量升高只出现在局部地区(H2O > 1-1.2 wt%)。火成岩矿物置换导致晶粒尺寸从 1 毫米减小到 ~10 μm。闪石表现出强烈的核心-边缘分带,主要受铁、镁和氢的高扩散性和铝的低扩散性控制。矿物成分平衡在 100-200 μm 尺度上实现。在毫米厚的局部剪切带和米级尺度的麦饭石闪长岩中,闪石(Ed0.2-0.5)和斜长石(An40-An80)的异质矿物成分表明,尽管流体-岩石比更高,流体渗流比偏长岩更普遍,但只有部分再平衡(在 200-500 μm 尺度上)。斜长石-闪石测温和平衡相图表明,最初的流体渗透和日冕形成是在800-850°C时通过沿晶界的断裂和渗流发生的。随后是主要的流体渗滤和绵延化事件,发生在 720-580°C 和约 4 千巴的排空和冷却过程中。裂缝中闪石的高(>300-400 ppm)氯(Cl)含量证明,在逆冲过程中,主要来自海水的流体涌入实现了持续的水化。断裂的异质分布从水化的最初阶段就开始控制流体的分布,从而产生正反馈作用,使含水矿物如闪石(相对于低应变区域,高应变区域的闪石含量高达+300 vol%)增长,并形成细粒混合域,导致粘性应变和质量传递进一步局部化(主要元素的变化为± 30-40%)。因此,Poroshiri蛇绿混杂岩是一个很好的化石实例,说明在海水衍生流体渗入到约15千米深的地方触发了变质和变形耦合过程的前跨压板块边界。
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引用次数: 0
Carboniferous Barrovian to Permian Buchan-type metamorphic cycles in the Mongolian Altai Zone: Implication for pressure cycles in accretionary orogens 蒙古阿尔泰区石炭纪巴罗维至二叠纪布坎型变质循环:对增生造山运动压力循环的影响
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-06-27 DOI: 10.1111/jmg.12777
Carmen Aguilar, Pavla Štípská, Karel Schulmann, Andrew R. C. Kylander-Clark, Ondrej Lexa, Turbold Sukhbaatar, Vít Peřestý, Yingde Jiang, Pavel Hanžl
<p>In the Altai Accretionary Wedge, several periods of Barrovian- and Buchan-type metamorphic cycles were dated from Ordovician to Permian. However, the timing and link between these cycles are not clear, and their causes are debated. In order to contribute to the understanding of Barrovian- to Buchan-type evolution of the accretionary wedges, we studied an area composed of three parallel belts in the easternmost extremity of the Hovd domain located in Mongolian Altai Zone: garnet gneiss in the north, garnet–staurolite–kyanite schist overprinted by ±sillimanite±cordierite±andalusite-bearing assemblages in the centre and garnet–sillimanite gneiss in the south. Petrography, garnet zoning and thermodynamic modelling indicate that the garnet gneiss from the northern belt records burial from ~510°C and ~3–4 kbar to ~600°C and ~5 kbar, followed by heating to ~660°C and decompression to ~4.5 kbar. The garnet–staurolite–kyanite schist from the central belt records burial from ~550°C and ~3–4.5 kbar to ~640–680°C and ~7 kbar, followed by decompression to the sillimanite stability field at ~650°C and ~6 kbar. Crystallization of cordierite, andalusite, late muscovite and chlorite in some samples indicates cooling on decompression to ~540°C and ~3.5 kbar. In the southern gneiss belt, the garnet–sillimanite gneiss with almost unzoned garnet suggests re-equilibration at ~6 kbar and ~710°C. In situ U–Pb monazite and xenotime dating carried out inclusions in porphyroblasts and matrix grains revealed Carboniferous and Permian ages. The monazite and xenotime from gneisses of the northern and southern belts record Carboniferous and Permian ages, which are interpreted as Carboniferous crystallization at c. 347 Ma associated with metamorphic peak, followed by Permian (re)crystallization at c. 300 and 283 Ma. In the central belt, rare Carboniferous xenotime grains in a garnet–staurolite–kyanite–andalusite–muscovite schist indicate a possible Carboniferous age of the prograde metamorphism. Predominant ages between c. 280 and 260 Ma recorded by monazite are interpreted as a result of complete recrystallization during an L<i>P</i> metamorphic overprint. The Carboniferous ages from the gneisses can be interpreted as constraining the timing of the exhumation of deep crustal rocks to shallow crustal levels. This event corresponds to the formation of crustal-scale migmatite-magmatite domes in the Mongolian Altai Zone. The prograde Barrovian assemblages in the central schist belt are interpreted as having formed contemporaneously during burial in a synform between the migmatite-magmatite domes. The Permian ages reflect L<i>P</i>–H<i>T</i> metamorphism, best recorded by the Buchan-type assemblages in the central schist belt, and are related to massive heat flux from tectonically mobile deep partially molten crust. Correlation with similar Barrovian- and Buchan-type episodes from the Chinese Altai Zone indicates multiple compressional and extensional events in the upper plate a
在阿尔泰断积楔,从奥陶纪到二叠纪发生了多次巴罗维变质周期和布坎变质周期。然而,这些周期的时间和之间的联系并不清楚,其原因也存在争议。为了帮助理解增生楔的巴罗维型到布坎型演化,我们研究了位于蒙古阿尔泰区霍夫德域最东端由三个平行带组成的区域:北部的石榴石片麻岩、中部由含±闪长岩±堇青石±安山岩集合体覆盖的石榴石-辉长岩-安山岩片岩和南部的石榴石-闪长岩片麻岩。岩相学、石榴石分带和热力学模型表明,北部岩带的石榴石片麻岩经历了从 ~510°C 和 ~3-4 千巴到 ~600°C 和 ~5 千巴的埋藏过程,随后加热到 ~660°C 并减压到 ~4.5 千巴。中央带的石榴石-白云石-榍石片岩记录了从~550°C和~3-4.5千巴到~640-680°C和~7千巴的埋藏过程,随后减压到~650°C和~6千巴的矽卡岩稳定场。一些样品中的堇青石、安托卢斯石、晚期蕈云母和绿泥石的结晶表明,减压至~540°C和~3.5千巴时冷却。在南部片麻岩带,石榴石-矽线石片麻岩中的石榴石几乎没有分带,这表明在~6千巴和~710°C时发生了再沸腾。对斑岩和基质颗粒中的包裹体进行的原位 U-Pb monazite 和 xenotime 测定显示了石炭纪和二叠纪的年龄。北部和南部片麻岩中的独居石和氙石记录了石炭纪和二叠纪的年龄,可解释为石炭纪结晶出现在约 347 Ma 与变质高峰有关的时期,随后二叠纪(再)结晶出现在约 300 和 283 Ma。在中央带,石榴石-陶土-黑云母-黄铁矿-木栓石片岩中罕见的石炭纪异时粒表明,顺层变质作用的年龄可能为石炭纪。独居石记录的主要年龄介于约 280 至 260 Ma 之间,被解释为 LP 变质叠加过程中完全重结晶的结果。片麻岩的石炭纪年龄可解释为制约了深地壳岩石向浅地壳水平掘出的时间。这一事件与蒙古阿尔泰区地壳规模的伟晶岩-伟晶岩穹窿的形成相吻合。中央片岩带中的原生巴罗维集合体被解释为在辉绿岩-伟晶岩穹窿之间的同步地层埋藏过程中同时形成的。二叠纪的年龄反映了 LP-HT 变质作用,中央片岩带的布坎型集合体对此有最好的记录,并与构造移动的深部部分熔融地壳的大量热流有关。与中国阿尔泰带类似的巴罗维期和布坎型事件的相关性表明,上板块增生楔中发生了多次压缩和延伸事件,可能与俯冲带的退缩和推进模式有关。
{"title":"Carboniferous Barrovian to Permian Buchan-type metamorphic cycles in the Mongolian Altai Zone: Implication for pressure cycles in accretionary orogens","authors":"Carmen Aguilar,&nbsp;Pavla Štípská,&nbsp;Karel Schulmann,&nbsp;Andrew R. C. Kylander-Clark,&nbsp;Ondrej Lexa,&nbsp;Turbold Sukhbaatar,&nbsp;Vít Peřestý,&nbsp;Yingde Jiang,&nbsp;Pavel Hanžl","doi":"10.1111/jmg.12777","DOIUrl":"10.1111/jmg.12777","url":null,"abstract":"&lt;p&gt;In the Altai Accretionary Wedge, several periods of Barrovian- and Buchan-type metamorphic cycles were dated from Ordovician to Permian. However, the timing and link between these cycles are not clear, and their causes are debated. In order to contribute to the understanding of Barrovian- to Buchan-type evolution of the accretionary wedges, we studied an area composed of three parallel belts in the easternmost extremity of the Hovd domain located in Mongolian Altai Zone: garnet gneiss in the north, garnet–staurolite–kyanite schist overprinted by ±sillimanite±cordierite±andalusite-bearing assemblages in the centre and garnet–sillimanite gneiss in the south. Petrography, garnet zoning and thermodynamic modelling indicate that the garnet gneiss from the northern belt records burial from ~510°C and ~3–4 kbar to ~600°C and ~5 kbar, followed by heating to ~660°C and decompression to ~4.5 kbar. The garnet–staurolite–kyanite schist from the central belt records burial from ~550°C and ~3–4.5 kbar to ~640–680°C and ~7 kbar, followed by decompression to the sillimanite stability field at ~650°C and ~6 kbar. Crystallization of cordierite, andalusite, late muscovite and chlorite in some samples indicates cooling on decompression to ~540°C and ~3.5 kbar. In the southern gneiss belt, the garnet–sillimanite gneiss with almost unzoned garnet suggests re-equilibration at ~6 kbar and ~710°C. In situ U–Pb monazite and xenotime dating carried out inclusions in porphyroblasts and matrix grains revealed Carboniferous and Permian ages. The monazite and xenotime from gneisses of the northern and southern belts record Carboniferous and Permian ages, which are interpreted as Carboniferous crystallization at c. 347 Ma associated with metamorphic peak, followed by Permian (re)crystallization at c. 300 and 283 Ma. In the central belt, rare Carboniferous xenotime grains in a garnet–staurolite–kyanite–andalusite–muscovite schist indicate a possible Carboniferous age of the prograde metamorphism. Predominant ages between c. 280 and 260 Ma recorded by monazite are interpreted as a result of complete recrystallization during an L&lt;i&gt;P&lt;/i&gt; metamorphic overprint. The Carboniferous ages from the gneisses can be interpreted as constraining the timing of the exhumation of deep crustal rocks to shallow crustal levels. This event corresponds to the formation of crustal-scale migmatite-magmatite domes in the Mongolian Altai Zone. The prograde Barrovian assemblages in the central schist belt are interpreted as having formed contemporaneously during burial in a synform between the migmatite-magmatite domes. The Permian ages reflect L&lt;i&gt;P&lt;/i&gt;–H&lt;i&gt;T&lt;/i&gt; metamorphism, best recorded by the Buchan-type assemblages in the central schist belt, and are related to massive heat flux from tectonically mobile deep partially molten crust. Correlation with similar Barrovian- and Buchan-type episodes from the Chinese Altai Zone indicates multiple compressional and extensional events in the upper plate a","PeriodicalId":16472,"journal":{"name":"Journal of Metamorphic Geology","volume":"42 7","pages":"979-1033"},"PeriodicalIF":3.5,"publicationDate":"2024-06-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/jmg.12777","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141501607","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Modification of the isotopic and geochemical compositions of accessory minerals controlled by microstructural setting 受微观结构环境控制的附属矿物同位素和地球化学成分的改变
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-06-22 DOI: 10.1111/jmg.12789
Chris Clark, Richard J. M. Taylor, Malcolm P. Roberts, Simon L. Harley

In situ age and trace element determinations of monazite, rutile and zircon grains from an ultrahigh temperature (UHT) metapelite-hosted leucosome from the Napier Complex using laser split-stream analysis reveal highly variable behaviour in both the U–Pb and trace element systematics that can be directly linked to the microstructural setting of individual grains. Monazite grains armoured by garnet and quartz retain two concordant ages 2.48 and 2.43 Ga that are consistent with the previously determined ages for peak UHT metamorphism in the Napier Complex. Yttrium in the armoured grains is unzoned with contents of ~700 ppm for the garnet-hosted monazite and in the range 400–1,600 ppm for the monazite enclosed within quartz. A monazite grain hosted within mesoperthite records a spread of ages from 2.43 to 2.20 Ga and Y contents ranging between 400 and 1,700 ppm. This grain exhibits core to rim zoning in both Y and age, with the cores enriched in Y relative to the rim and younger ages in the core relative to the rim. A monazite grain that sits on a grain boundary between mesoperthite and garnet records the largest spread in ages—from 2.42 to 2.05 Ga. The youngest ages in this grain are within a linear feature that reaches the core and is connected to the grain boundary between the garnet and mesoperthite; the oldest ages are observed where monazite is in contact with garnet. Yttrium in the grain is enriched in the core and depleted at the rim with the strongest depletions where monazite is adjacent to grain boundaries between the silicate minerals or in contact with garnet. The unarmoured monazite grains have lower intercept ages of 1.85 Ga, which overlaps with the bulk of ages determined from the rutile and is coincident with a previously reported zircon age obtained through depth profiling from the Napier Complex. The age and chemical relationships outlined above illustrate decoupling between the geochemical and geochronological systems in monazite. Individual grains are suggestive of a range of processes that modify these systems, including volume diffusion, flux-limited diffusion and fluid-enhanced recrystallization, all operating at the scale of a single thin section and primarily controlled by host mineral microstructural setting. These findings illustrate how the development of simple partitioning coefficients (cf. garnet/zircon) and geospeedometry based on experimentally determined diffusion coefficients on grain separates may not be achievable. However, it highlights the utility of combining age and trace element concentrations from multiple accessory minerals with microstructural information when trying to build a complete history of tectonothermal events experienced by an ancient rock system that has undergone a prolonged history of thermal, deformational and fluid flow events.

利用激光分流分析法对来自纳皮尔岩群的超高温(UHT)元青石寄主白铁矿的独居石、金红石和锆石晶粒进行了原位年龄和痕量元素测定,结果表明,U-Pb和痕量元素系统学的行为变化很大,这与单个晶粒的微观结构环境直接相关。被石榴石和石英铠装的独居石晶粒保留了两个一致的年龄 2.48 Ga 和 2.43 Ga,与之前测定的纳皮尔岩群超高温变质峰值年龄一致。铠装晶粒中的钇未分区,石榴石包裹的独居石中的钇含量为约 700 ppm,石英包裹的独居石中的钇含量为 400-1,600 ppm。中透辉石中寄生的独居石晶粒记录的年龄从 2.43 Ga 到 2.20 Ga 不等,Y 含量在 400 ppm 到 1,700 ppm 之间。该晶粒在Y和年龄方面都呈现出从岩芯到岩缘的分带,岩芯的Y含量相对于岩缘更高,岩芯的年龄相对于岩缘更年轻。位于中透辉石和石榴石晶界上的一个独居石晶粒记录了最大的年龄分布--从 2.42 Ga 到 2.05 Ga。该晶粒中最年轻的年龄位于一个线性特征内,该线性特征直达晶核,并与石榴石和中透辉石之间的晶界相连;最古老的年龄出现在独居石与石榴石接触的地方。晶粒中的钇在核心富集,在边缘贫化,在独居石邻近硅酸盐矿物之间的晶界或与石榴石接触的地方贫化最严重。未铠装独居石晶粒的截距年龄较低,为 1.85 Ga,这与从金红石中测定的大部分年龄相重叠,并且与之前报告的通过纳皮尔复合体深度剖面获得的锆石年龄相吻合。上述年龄和化学关系说明了独居石的地球化学和地质年代系统之间的脱钩。单个晶粒表明了改变这些系统的一系列过程,包括体积扩散、通量限制扩散和流体强化再结晶,所有这些过程都是在单个薄片的尺度上进行的,并且主要受主矿物微结构环境的控制。这些发现说明,根据实验确定的晶粒分离扩散系数来制定简单的分区系数(如石榴石/锆石)和地质速度测定法可能是无法实现的。不过,这也凸显了将多种附属矿物的年龄和痕量元素浓度与微观结构信息结合起来,在试图建立一个经历了长期热、变形和流体流动事件的古老岩石系统所经历的构造热事件的完整历史时的实用性。
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引用次数: 0
Hydrous shear zones are sites of melt transfer in the lower arc crust: A case study from Fiordland, New Zealand 含水剪切带是下弧地壳熔体转移的场所:新西兰峡湾地区的案例研究
IF 3.5 2区 地球科学 Q1 GEOLOGY Pub Date : 2024-06-19 DOI: 10.1111/jmg.12788
Aditi Chatterjee, Nathan R. Daczko, Joyjit Dey, Sandra Piazolo

Recent studies of the Cretaceous lower arc crust exposed in Fiordland, New Zealand, conclude that shear zones are sites of melt migration and mass transfer through the deep crust. Here, we investigate the 4–10 km-wide George Sound Shear Zone, which cuts the Western Fiordland Orthogneiss, comprising two main rock types: two-pyroxene gneiss and hornblende gneiss. Previous studies infer a predominantly igneous origin for the two types of gneiss. However, this study finds that melt-rock interaction within the George Sound Shear Zone formed the hornblende gneiss from the precursor two-pyroxene gneiss. Petrographic analyses of samples collected in transects across the shear zone show hydration reaction textures ranging from rims of hornblende + quartz around pyroxene grains to complete replacement of pyroxene grains. Plagioclase is recrystallized and partially replaced by clinozoisite. Additionally, biotite mode increases towards the higher strain rocks in the shear zone. Backscatter images and polarized light microscopy show microstructures indicative of former melt-present deformation, including (a) interconnected mineral films of quartz and K-feldspar along grain boundaries, (b) grains that terminate with low apparent dihedral angles, (c) interstitial grains, with some (d) undulose extinction in plagioclase and (e) serrated grain boundaries. In addition, zircon microstructures are consistent with Zr mobility, further supporting the former presence of melt; geochemical data show enrichment of Zr in the hornblende gneiss as compared to the two-pyroxene gneiss. From the above observations, it is inferred that a felsic to intermediate hydrous melt migrated through the George Sound Shear Zone reacting with the host two-pyroxene gneiss of the Western Fiordland Orthogneiss. Melt migration along grain boundaries was deformation assisted, (i) causing hydration of pyroxene to hornblende + quartz, and plagioclase to clinozoisite, (ii) increasing proportions of biotite within the shear zone and (iii) causing depletion of Cr + Ni and Zr enrichment in the hydrated rock. Our interpretation is supported by published observations of pegmatite dyke swarms that intruded into the George Sound Shear Zone, the P-T conditions of deformation and characterization of microstructures that contrast sharply with those typically found in mylonitic rocks formed under solid-state metamorphic conditions. Our results confirm that hydrous shear zones within otherwise anhydrous country rock are retrogressive and may represent evidence of melt migration through zones of deformation.

最近对新西兰峡湾地区出露的白垩纪下弧地壳进行的研究得出结论,剪切带是地壳深处熔体迁移和质量转移的场所。在这里,我们研究了 4-10 公里宽的乔治湾剪切带,该剪切带切割了西峡湾正长片麻岩,由两种主要岩石类型组成:双辉石片麻岩和角闪石片麻岩。之前的研究推断这两种片麻岩主要起源于火成岩。然而,本研究发现,乔治湾剪切带内的熔岩相互作用形成了角闪石片麻岩,而角闪石片麻岩的前身是双辉石片麻岩。在剪切带横断面上采集的样品的岩相分析表明,水化反应纹理从辉石晶粒周围的角闪石+石英边缘到辉石晶粒的完全置换不等。斜长石被重结晶,部分被黝帘石取代。此外,在剪切带的高应变岩石中,斜长石模式有所增加。背散射图像和偏振光显微镜显示了表明以前熔体存在变形的微观结构,包括(a)沿晶界的石英和钾长石相互连接的矿物膜;(b)以低表观二面角终止的晶粒;(c)间隙晶粒,以及(d)斜长石中的一些波状消光;(e)锯齿状晶界。此外,锆石的微观结构与锆元素的流动性相一致,进一步证明了熔体的存在;地球化学数据显示,角闪石片麻岩中的锆元素比二辉石片麻岩中的富集。根据上述观察结果,可以推断出长英质至中等含水熔体穿过乔治湾剪切带,与西峡湾正长片麻岩的主质双辉石片麻岩发生反应。熔体沿晶界的迁移是在变形的辅助下进行的,(i) 使辉石水合为角闪石+石英,斜长石水合为黝帘石,(ii) 增加了剪切带中生物橄榄石的比例,(iii) 使水合岩石中的铬+镍和锆富集。我们的解释得到了对侵入乔治湾剪切带的伟晶岩岩体群、变形的 P-T 条件和微观结构特征的公开观察结果的支持,这些微观结构特征与在固态变质条件下形成的岩浆岩中通常发现的微观结构形成了鲜明对比。我们的研究结果证实,原本无水的乡村岩石中的水化剪切带是逆行的,可能是熔体通过变形区迁移的证据。
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Journal of Metamorphic Geology
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