[논문]영남육괴에 기록된 고원생대 고온조산운동

이유영; 조문섭

doi:10.22807/kjmp.2022.35.3.199

영남육괴에 기록된 고원생대 고온조산운동
Paleoproterozoic Hot Orogenesis Recorded in the Yeongnam Massif, Korea 원문보기

광물과 암석 = Korean journal of mineralogy and petrology, v.35 no.3, 2022년, pp.199 - 214

이유영 (한국기초과학지원연구원 환경분석연구부) , 조문섭 (서울대학교 지구환경과학부)

초록
AI-Helper

영남육괴는 광역적인 고온-저압의 변성작용과 부분용융을 경험한 한반도 지각을 대표하는 기반암 중 하나이다. 이 논문에서는 지금까지 보고된 영남육괴 고온 변성암류에 기록된 백립암상의 변성작용과 부분용융 과정을 통해 고원생대(1.87-1.84Ga)의 고온조산운동 기록을 살펴본다. 특히 열원으로서의 역할을 담당했던, 산청-하동지역 회장암질 마그마를 비롯한 고철질 화성활동과 고온-저압 변성작용 사이의 시공간적 연계는 영남육괴의 광역변성작용과 지각용융을 이해하는데 필수적인 정보를 제공한다. 지각용융은 주로 함(含)유체 부분용융과 백운모/흑운모의 탈수용융에 의해 발생하였으며, 다양한 형태의 우백대와 우백질 화강암을 형성하였다. 이차이온질량분석기를 활용한 저어콘과 모나자이트의 암석연대학적 결과는 영남육괴의 고온변성작용과 부분용융이 약 1870-1854 Ma의 ~15 Ma 기간 동안 지속되었음을 지시한다. 또한, 초기 차노카이트로 대표되는 유체유입 사건이 약 1840 Ma에 발생하였다. 이와 같이 영남육괴 내에는 고온변성작용과 부분융용, 그리고 유체유입이라는 고온조산대를 대표하는 일련의 지질사건들이 기록되어 있다. 영남육괴에서 확인된 고온조산대는 북중국 지괴에서 흔히 보고되는 고원생대 조산운동과 연계되어 있으며, 고원생대 콜럼비아/누나 초대륙 진화의 최후기 산물이리라 판단된다.

Abstract ▼ AI-Helper

The Yeongnam Massif is one of representative basement provinces in the Korean Peninsula, which has experienced high-temperature, low-pressure (HTLP) regional metamorphism and partial melting. Here we reviewed recent developments in Paleoproterozoic (1.87-1.84 Ga) hot orogenesis of the Yeongnam Massif, typified by the granulite-facies metamorphism and partial melting recorded in the HTLP rocks. In particular, spatiotemporal linkage between the metamorphic and magmatic activities, including the Sancheong-Hadong anorthositic magma as a heat source, provides a key to understand the widespread HTLP metamorphism and partial melting in the Yeongnam Massif. Crustal anatexis, resulting from the fluid-present melting and muscovite/biotite dehydration melting, has yielded various types of leucosomes and leucogranites. Zircon and monazite petrochronology, using in-situ U(-Th)-Pb data from the secondary ion mass spectrometry, indicates that the HTLP metamorphism and anatexis lasted over a period of ~15 Ma at ca. 1870-1854 Ma. In addition, a fluid influx event at ca. 1840 Ma was locally recognized by the occurrence of incipient charnockite. Taken together, the Yeongnam Massif preserves a prolonged evolutionary record of the HTLP metamorphism, partial melting, and fluid influx diagnostic for a hot orogen. Such an orogen is linked to the Paleoproterozoic orogeny widespread in the North China Craton, and most likely represents the final phase of crustal evolution in the Columbia/Nuna supercontinent.

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표/그림 (5)

그림 Fig. 1. (a) Simplified tectonic province map of East Asia (modified after Cho et al., 2017). The area shown in the box is enlarged in (b). (b) Geological map of the Yeongnam Massif showing the compilation of SHRIMP zircon and monazite ages and P-T data (modified after Lee et al., 2018). Note that the Yeongnam Massif is unconformably overlain by early and late Paleozoic sedimentary strata of the Taebaeksan Basin, shown in blue; such stratigraphic relationship is diagnostic for the North China Craton affinity. The SHRIMP zircon and monazite ages (red, igneous; blue, metamorphic) of basement gneisses are illustrated together with individual references: (a) Cho et al. (2020); (b) Lee et al. (2019); (c) Lee et al. (2020); (d) Lee et al. (2010); (e) Kim et al. (2009); (f) Kim et al. (2012); (g) Kim et al. (2014a); (h) Lee et al. (2014); (i) Lee and Cho (2020); (j) Lee and Cho (2012); (k) Lee et al. (2017b); (l) Kim et al. (2014b); (m) Lee et al. (2017a); (n) Lee et al. (2018); and (o) Lee et al. (2021). P-T conditions estimated from the gneisses are also shown together with references: (1) Song (1999); (2) Kwon et al. (2003); (3) Kim and Cho (2003); (4) Cheong and Na (2008); (5) Lee and Cho (2020); (6) Lee et al. (2017a); (7) Lee et al. (2018); and (8) Lee et al. (2020).
그림 Fig. 2. Field photographs of high-temperature gneisses and a migmatitic amphibolite. (a) Light-colored leucosome in pelitic migmatite, aligned subparallel to the foliation. The leucosome has indistinct or slightly diffused boundaries. (b) Rounded, elongate psammitic schollens distributed in pelitic diatexite subparallel to the foliation. Large garnet porphyroblasts are abundant in the pelitic diatexite. (c) Dilation structures apparently governing the distribution of leucosomes and biotite-rich selvedges in the garnet-orthopyroxene granulite. (d) A network of in-situ, layer-parallel, and interboudin leucosomes in semipelitic migmatite where large garnet porphyroblasts are common. (e) A network of leucosomes in psammitic migmatite showing the diffused boundary with the host, and a wider leucosome vein consisting of coarse-grained quartz and feldspar, together with large cordierite porphyroblasts, in semipelitic migmatite. (f) Leucosomes in the Okbang amphibolite generally oriented subparallel to major foliation and concentrated at boudin necks.
그림 Fig. 3. Compilation of P-T paths reported from the Yeongnam Massif. Four thermal gradients of 1500℃/GPa, 775℃/GPa, 375℃/GPa, and 150℃/GPa, respectively, are shown together with the three types of metamorphic regions typified by high, intermediate, and low dP/dT gradients (Brown and Johnson, 2018). Also shown are approximate solidus regions of the dehydration melting of muscovite and biotite, respectively (Weinberg and Hasalová, 2015), and the phase equilibria among the Al-silicates of kyanite (Ky), sillimanite (Sil), and andalusite (And).
그림 Fig. 4. Timelines illustrating progressive episodes of high-temperature, low-pressure metamorphism and local fluid influx in the Sancheong-Hadong complex (modified after Lee et al., 2018). The probability curve based on zircon U-Pb ages from the AMCG suite (Lee et al., 2014, 2017a, b, 2021; Kim et al., 2014b) is shown in green dotted curve. Vertical bars denote the age ranges, including 2σ uncertainties, of the analyzed samples.
그림 Fig. 5. Age distribution histograms of zircon (and monazite) in (a) igneous and (b) metamorphic rocks (Data sources are the same as those given in Fig. 1b). The bin widths are 20 m.y., and relative age probability curves are also shown.

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