まとめ
地震屈折データにより,中国の云南省の大陸の正常な地殻構成が明らかになった. これは,海洋の島弧の蓄積ではなく,堆積過程が,この地域を形成したことを示唆しています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- テクトニクス (地質学) とは
- 地球科学 地球科学 地球科学
背景:
- 雲南省は,ヒマラヤ・ビルマ弧の南端にある地質学的に活発である.
- 地殻の構造を理解することは,地域構造の進化の解読の鍵です.
研究 の 目的:
- 地震屈折を用いて云南省の地殻構造を定義する.
- この地域の地殻の構成と進化の歴史を推論する.
主な方法:
- 地震屈折プロフィールは,雲南省で行われました.
- 地震波の速度を分析し,地殻の厚さや組成を決定する.
主要な成果:
- 地殻の厚さは38キロから46キロメートルに及ぶ.
- 低平均地殻速度は,メタ堆積物とシリシックの侵入性岩の組成を示しています.
- 1つのプロファイルで異常に低い上部マントルの速度が観測され,潜在的なマントルの活動または地震性アニソトロピーを示唆しました.
結論:
- この地殻の組成は,長江平面の側面の堆積過程を含む進化モデルを支持している.
- この発見は,この地域における海洋島の弧積層に関する以前の仮説に異議を唱えている.
- 上層マントルの潜在的に活発な地形構造プロセスや地震性アニソトロピーについては,さらなる調査が必要である.
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