Development of migmatites and the role of viscous segregation in high-T metamorphic complexes: Example from the Ryoke Metamorphic Complex, Mikawa Plateau, Central Japan

被引:20
|
作者
Miyazaki, Kazuhiro [1 ]
机构
[1] Geol Survey Japan AIST, Tsukuba, Ibaraki 3058567, Japan
关键词
High-T metamorphism; Migmatite; Melt migration; Ryoke Metamorphic Complex; Simple-shear deformation; Viscous segregation; PARTIALLY MOLTEN ROCKS; SYNTECTONIC MELT PATHWAYS; KARAKORAM SHEAR ZONE; SOUTHWEST JAPAN; MAGMA MIGRATION; OROGENIC BELTS; GRANITE MAGMA; NW INDIA; DEFORMATION; EMPLACEMENT;
D O I
10.1016/j.lithos.2009.11.012
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Ryoke Metamorphic Complex of the Mikawa Plateau, Central Japan, contains well-preserved geological and thermal structures formed during Cretaceous high-temperature (high-T) metamorphism. These structures can be explained by a pervasive melt migration model. However, the estimated flux of melt is much higher than that expected for compaction flow of felsic melt. An additional tectonic force and/or melt segregation to network of veins or layers is therefore required. This paper presents the results of numerical modeling of the structural evolution of immiscible viscous fluids under simple-shear deformation, and discusses the role of viscous segregation in enabling pervasive melt flow in hot crust. The results of numerical modeling of simple-shear deformation of immiscible viscous fluids reveal that low-viscosity fluids segregate into lenses and layers. This segregation is a type of viscous segregation that takes place to minimize the dissipation of energy in the system. The rate of energy dissipation is proportional to viscosity. Therefore, this process is expected to occur universally in immiscible viscous fluids with large viscosity contrasts, and is an important process in focusing melt in partially melted rocks. The structures produced by the numerical simulation are similar to those of migmatites. The simulation results suggest that melts distributed randomly in partially melted rock will segregate into lenses or layers with progressive simple-shear deformation. During deformation-enhanced segregation, a melt network will form dynamically. If this process occurs at small to large scales in the hot crust, melts will be effectively transported upward due to buoyancy forces. It is possible that pervasive migmatites at low structural levels within high-T metamorphic complexes may represent "fossil" melt pathways formed by crustal-scale viscous segregation. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:287 / 299
页数:13
相关论文
共 21 条
  • [1] The Ryoke metamorphic belt (Japan): An excellent example of low-P/high-T metamorphic belt
    Okudaira, T
    [J]. GONDWANA RESEARCH, 1997, 1 (01) : 147 - 148
  • [2] Polymetamorphism in high-T metamorphic rocks: An example from the central Appalachians
    Broadwell, Kirkland S.
    Caddick, Mark J.
    Beard, James S.
    [J]. JOURNAL OF METAMORPHIC GEOLOGY, 2019, 37 (09) : 1209 - 1234
  • [3] Kinetics and pulses of zircon growth in migmatites beneath a volcanic arc: An example from the high-T Ryoke Complex, southwest Japan
    Miyazaki, Kazuhiro
    Ikeda, Takeshi
    Iwano, Hideki
    Hirata, Takafumi
    Danhara, Tohru
    [J]. JOURNAL OF METAMORPHIC GEOLOGY, 2023, 41 (05) : 639 - 664
  • [4] A high-T metamorphic complex derived from the high-P Suo metamorphic complex in the Omuta district, northern Kyushu, southwest Japan
    Miyazaki, Kazuhiro
    Ikeda, Takeshi
    Matsuura, Hirohisa
    Danhara, Tohru
    Iwano, Hideki
    Hirata, Takafumi
    [J]. ISLAND ARC, 2017, 26 (05)
  • [5] Tourmaline and boron as indicators of the presence, segregation and extraction of melt in pelitic migmatites: examples from the Ryoke metamorphic belt, SW Japan
    Kawakami, T
    [J]. TRANSACTIONS OF THE ROYAL SOCIETY OF EDINBURGH-EARTH SCIENCES, 2004, 95 : 111 - 123
  • [6] Tourmaline and boron as indicators of the presence, segregation and extraction of melt in pelitic migmatites: examples from the Ryoke metamorphic belt, SW Japan
    Kawakami, Tetsuo
    [J]. FIFTH HUTTON SYMPOSIUM ON THE ORIGIN OF GRANITES AND RELATED ROCKS, 2004, 389 : 111 - 123
  • [7] CHIME monazite dating as a tool to detect polymetamorphism in high-temperature metamorphic terrane: Example from the Aoyama area, Ryoke metamorphic belt, Southwest Japan
    Kawakami, Tetsuo
    Suzuki, Kazuhiro
    [J]. ISLAND ARC, 2011, 20 (03) : 439 - 453
  • [8] The metamorphic evolution of migmatites from the Otztal Complex (Tyrol, Austria) and constraints on the timing of the pre-Variscan high-T event in the Eastern Alps
    Thoeny, Werner F.
    Tropper, Peter
    Schennach, Friederike
    Krenn, Erwin
    Finger, Friedrich
    Kaindl, Reinhard
    Bernhard, Franz
    Hoinkes, Georg
    [J]. SWISS JOURNAL OF GEOSCIENCES, 2008, 101 (Suppl 1) : S111 - S126
  • [9] The metamorphic evolution of migmatites from the Ötztal Complex (Tyrol, Austria) and constraints on the timing of the pre-Variscan high-T event in the Eastern Alps
    Werner F. Thöny
    Peter Tropper
    Friederike Schennach
    Erwin Krenn
    Friedrich Finger
    Reinhard Kaindl
    Franz Bernhard
    Georg Hoinkes
    [J]. Swiss Journal of Geosciences, 2008, 101 : 111 - 126
  • [10] Denudation history of the high T/P Ryoke metamorphic belt, southwest Japan: constraints from CHIME monazite ages of gneisses and granitoids
    Suzuki, K
    Adachi, M
    [J]. JOURNAL OF METAMORPHIC GEOLOGY, 1998, 16 (01) : 23 - 37