Devonian Andean-type convergence in the southern Dunhuang block (NW China): Petro-structural, metamorphic P–T and geochronological constraints

IF 3.5 2区 地球科学 Q1 GEOLOGY
Jérémie Soldner, Yingde Jiang, Pavla Štípská, Karel Schulmann, Chao Yuan, Zongying Huang, Yunying Zhang
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引用次数: 0

Abstract

Archean to Palaeoproterozoic basement rocks exposed in the Dunhuang block in NW China were affected by Palaeozoic crustal reworking, as constrained by previous zircon U–Pb geochronological investigations. However, relationships between the Palaeozoic metamorphic ages, P–T evolution and deformational history of the region remain ambiguous. In order to address this issue, P–T–t–D paths of paragneisses from the basement of the Hongliuxia belt in the southern Dunhuang block were investigated. Inclusions in garnet and kyanite from the paragneisses are considered as vestiges of Palaeozoic M1 metamorphism corresponding to initiation of the prograde evolution. The earliest continuous metamorphic fabric is an originally steep N–S striking foliation S2. This fabric was reworked by vertical folds F3 associated with the development of a ubiquitous steep, mainly south-dipping, E-W striking axial planar foliation S3. The S2 foliation in paragneisses is mainly associated with Grt–St–Ky–Sil–Bt–Ms–Pl–Qz–Rt assemblages in samples from the western domain and with Grt–Ky–Sil–Bt–Kfs–Pl–Qz–Rt assemblages in samples from the northeastern domain of the Hongliuxia belt. The S3 foliation is associated with Grt–Sil–St–Bt–Ms–Pl–Qz–Ilm assemblages in the western domain and with Grt–Sil–Bt–Ms–Pl–Qz–Kfs–Ilm assemblages in the northeastern domain, followed by growth of chlorite in both domains. Early prograde stage (M1) from 4.0–6.5 kbar and 540–560°C to metamorphic peak (M2a) at 9–10 kbar and ~650–675°C is mainly recorded by paragneisses from the western domain. Subsequent decompression is initially accompanied by heating (M2b) constrained to 6.5–7 kbar and 675–710°C in the western domain, and to 6–6.5 kbar and ~730°C in the northeastern domain, followed by cooling (M3) through 4–6.5 kbar and 550–650°C till late chloritization (late M3). In situ U–Pb dating of monazite combined with monazite trace-element compositions suggests that prograde evolution (M1) most likely started at c. 406 Ma, peak-P conditions (M2a) were reached at 400–394 Ma, decompression associated with heating (M2b) took place at 393–391 Ma, and cooling (M3) during exhumation probably lasted from 380 to 354 Ma. The prograde metamorphism probably reflects burial during underthrusting of neighbouring continental basement (the Alxa block or an equivalent) below the Dunhuang block. This event culminated in pure shear thickening (D2a) of the whole supra-subduction margin followed by minor heating and exhumation (D2b). The D3-M3 event is interpreted as reflecting exhumation during orthogonal shortening of the system, possibly in response to an independent orogenic cycle. Combined with the available regional data, this study reveals the existence of a complex tectono-metamorphic evolution for the Dunhuang block characterized by two distinct orogenic phases with (i) the thickening of a previously thinned arc-back-arc crust recorded in the northern and central belts at 420–410 Ma in the pro-wedge side of the active margin (Sanweishan phase), followed by (ii) the 410–390 Ma thickening in the retro-wedge side (Hongliuxia phase). Such a tectonic evolution of the whole Dunhuang block resembles Andean-type migration of crustal thickening from the convergent front to hinterlands. The D3-M3 event, potentially responsible for the juxtaposition of rocks from different geological occurrences and depths, is seemingly independent from this Andean-type orogenic cycle.

敦煌南地块(中国西北部)泥盆系安第斯型汇聚:岩石结构、变质P-T和地质年代制约因素
根据以往的锆石U-Pb地质年代研究,中国西北部敦煌地块出露的奥陶系至古近纪基底岩石受到了古生代地壳再加工的影响。然而,该地区古生代变质年龄、P-T演化和变形史之间的关系仍然模糊不清。为了解决这一问题,研究了敦煌南块红柳峡带基底副片麻岩的P-T-t-D路径。副片麻岩中的石榴石和黝帘石包体被认为是古生代M1变质作用的遗迹,对应于顺演化的开始。最早的连续变质构造是原本陡峭的 N-S 向褶皱 S2。该构造经垂直褶皱 F3 的再加工,形成了无处不在的陡峭的、主要向南倾斜的、东西走向的轴向平面褶皱 S3。S2褶皱在片麻岩中主要与红柳峡带西部岩域样品中的Grt-St-Ky-Sil-Bt-Ms-Pl-Qz-Rt组合以及东北部岩域样品中的Grt-Ky-Sil-Bt-Kfs-Pl-Qz-Rt组合有关。S3褶皱与西域的Grt-Sil-St-Bt-Ms-Pl-Qz-Ilm集合体有关,与东北域的Grt-Sil-Bt-Ms-Pl-Qz-Kfs-Ilm集合体有关,随后绿泥石在这两个域中生长。从4.0-6.5千巴和540-560°C的早期顺行阶段(M1)到9-10千巴和约650-675°C的变质高峰(M2a),主要记录在西部岩域的片麻岩中。随后的减压最初伴随着加热(M2b),在西部岩域为6.5-7千巴和675-710°C,在东北部岩域为6-6.5千巴和~730°C,随后冷却(M3)至4-6.5千巴和550-650°C,直至后期绿泥石化(M3晚期)。独居石的原位U-Pb年代测定与独居石痕量元素成分相结合,表明顺行演化(M1)很可能始于约406Ma,P峰值条件(M2a)在400-394Ma达到,与加热相关的减压(M2b)发生在393-391Ma,出露过程中的冷却(M3)可能持续了380-354Ma。顺行变质作用可能反映了敦煌地块下方邻近大陆基底(阿拉善地块或类似地块)在下推过程中的埋藏作用。这一事件的高潮是整个超俯冲边缘的纯剪切增厚(D2a),随后是轻微的加热和掘起(D2b)。D3-M3事件被解释为反映了该系统正交缩短过程中的掘起,可能是对独立造山周期的回应。结合现有的区域数据,这项研究揭示了敦煌块体存在着复杂的构造-变质演化过程,其特征是两个不同的造山运动阶段:(i)在活动边缘的前缘一侧,北带和中带在 420-410 Ma 时记录到先前变薄的弧-弧地壳增厚(三尾山阶段);(ii)在后缘一侧,在 410-390 Ma 时记录到地壳增厚(红柳峡阶段)。整个敦煌块体的这种构造演化类似于安第斯型地壳增厚从汇聚前沿向腹地的迁移。D3-M3事件可能导致不同地质构造和深度的岩石并置,但似乎独立于安第斯型造山运动周期。
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来源期刊
CiteScore
6.60
自引率
11.80%
发文量
57
审稿时长
6-12 weeks
期刊介绍: The journal, which is published nine times a year, encompasses the entire range of metamorphic studies, from the scale of the individual crystal to that of lithospheric plates, including regional studies of metamorphic terranes, modelling of metamorphic processes, microstructural and deformation studies in relation to metamorphism, geochronology and geochemistry in metamorphic systems, the experimental study of metamorphic reactions, properties of metamorphic minerals and rocks and the economic aspects of metamorphic terranes.
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