Về cơ chế va chạm giữa Ấn Độ và Á Châu
Tóm tắt
Các nghiên cứu thực địa về đứt gãy hoạt động ở Nam Tây Tạng cho thấy rằng sự giãn nở ở Thế Đệ Tứ đã diễn ra với tốc độ khoảng ≃1 cm mỗi năm theo hướng ≃ 100°. Điều này ngụ ý rằng việc đẩy chìm ở Himalaya hiện hấp thụ ít hơn một nửa tổng độ hội tụ giữa Ấn Độ cứng và Á Châu, phần còn lại chủ yếu được hấp thụ bằng cách đứt gãy trượt trái phía Bắc của đới va chạm. Các đứt gãy trượt phải,
Từ khóa
Tài liệu tham khảo
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