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J4 ›› 2012, Vol. 18 ›› Issue (2): 280-.

• 其他学科论文 • 上一篇    下一篇

波罗的与西伯利亚板块古生代运动学特征对比新认识

傅臣建,李江海   

  1. 北京大学 地球与空间科学学院;造山带与地壳演化教育部重点实验室,北京
  • 出版日期:2012-06-20 发布日期:2012-07-11
  • 作者简介:傅臣建, 男, 1986年生, 在读研究生, 构造地质学专业; E-mail: fuchenjian@pku.edu.cn

New Understanding From Comparison of Paleozoic Kinematics
Between Baltica and Siberia

FU Chenjian, LI Jianghai   

  1. School of Earth and Space Sciences, Peking University;
    The Key Laboratory of Orogenic Belt and Crust Evolution, Ministry of Education, Beijing
  • Online:2012-06-20 Published:2012-07-11

摘要:

       古地磁学是进行古板块运动演化过程和古地理重建研究最有效的定量方法之一。在统计全球古地磁数据库(GPMDB)
和前人发表数据的基础上,根据国际上通用的古地磁数据可靠性判别标准——Van der Voo (1990)判据,本文对波罗的板
块(Baltica)和西伯利亚板块(Siberia)古生代古地磁数据进行了重新分析和筛选,利用GMAP 软件重建了两个板块古生代
视极移曲线和古地理方位,对它们的构造演化和运动学特征进行对比分析,获得了几点新认识,即两板块在古生代期间发
生的三次汇聚(晚奥陶世、早石炭世和晚二叠世)过程符合牛顿运动学原则(板块之下是具有很大粘度的地幔软流圈,非
理想条件下不可能完全遵守牛顿运动学原则),且具有三种不同类型的运动学现象:晚奥陶世(~450 Ma),波罗的和西伯利
亚板块同向北漂移并汇聚,纬向速度较快的板块波罗的将动能传给了纬向速度较慢的西伯利亚板块;早石炭世(~360 Ma),
波罗的和西伯利亚板块相向漂移并汇聚,西伯利亚板块向南的板块纬向速度转为向北,波罗的板块向北的纬向速度逐渐减
小并转为向南;晚二叠世(~255 Ma),波罗的和西伯利亚板块再次相向漂移并汇聚,动能抵消,纬向漂移速率都变为零。

关键词: 波罗的和西伯利亚板块, 古地磁, 运动学原则, 视极移曲线, 纬向漂移速率, 旋转速率

Abstract:

       Paleomagnetism is one of the most effective quantitative methods for examining ancient plate tectonic evolution and
paleogeographic reconstructions. Based on data from the Global Paleomagnetic Database (GPMDB 4.6) and previously published
paleomagnetic data for the Baltic and Siberian plates, a reanalysis and filtering of Baltica and Siberia Paleozoic paleomagnetic
data has been performed in accordance with internationally accepted basic selection criteria (Van der Voo, 1990) determining
the reliability of paleomagnetic data. From this, a reconstruction of the apparent polar wander paths (APWP) and paleogeographic
positions of the Baltic and Siberian plates has been made by using the GMAP software. In addition, further analysis has been
made by comparing the structural evolution and kinematic characteristics. In conclusion, the following is understood for these two
plates during the Paleozoic. Three convergence events took place during the Late Ordovician (~450 Ma), Early Carboniferous (~360
Ma), and Late Permian (~255 Ma), and the processes of plate convergence follow Newtonian kinematic principles in general.
What needs to be stressed is that under the continental plates is the asthenosphere mantle with an extremely high viscosity, so the
Newtonian kinematic principles cannot be obeyed under non-ideal conditions. Three processes of plate convergence have three
different kinematic phenomena. During the late Ordovician (~450 Ma), both Baltica and Siberia drifted northward and converged
gradually. Baltica with higher latitudinal velocity converted its kinetic energy into Siberia with lower latitudinal velocity. Duringthe Early Carboniferous (~360 Ma), Baltica and Siberia moved towards each other and converged. The latitudinal drift direction
of Siberia changed from the south to the north while the latitudinal velocity of Baltica decreased and became toward the south
gradually. During the Late Permian (~255 Ma), Baltica and Siberia drifted towards each other and converged again. Finally, their
kinetic energy canceled out each other, so both latitudinal velocities became zero.

Key words: Baltica, Siberia, paleomagnetism, kinematic principles, apparent polar wander path, latitudinal drift-rate, angular
rotation

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