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Đặc điểm địa chất của các đới biến chất siêu cao áp kiểu đại dương và những ý nghĩa kiến tạo: Nghiên cứu trường hợp từ Tây Nam Thiên Sơn và Bắc Côn Đảo ở phía Tây Bắc Trung Quốc
Tóm tắt
Bài báo này tổng hợp các đặc điểm địa chất của các đới biến chất siêu cao áp (UHP) hình thành từ sự hụt nén sâu của vỏ đại dương. Đới biến chất UHP kiểu đại dương được đặc trưng bởi thành phần protolith là vỏ đại dương điển hình, nhiệt độ biến chất cao nhất <600°, quỹ đạo P-T trải qua trạng thái biến chất blueschist trong quá trình tiến triển và thoái trào của quá trình biến chất, tương ứng, với gradient địa nhiệt thấp của sự hụt nén lạnh. Nghiên cứu sâu hơn về đới biến chất UHP kiểu đại dương là rất cần thiết để xây dựng chuỗi phản ứng biến chất của vùng hụt nén lạnh, để hiểu cách mà các chất lỏng chứa nước được vận chuyển vào sâu trong manti và để phân loại các loại biến chất UHP trong vùng hụt nén lạnh. Cơ chế nâng cao và khai thác các đá biến chất UHP kiểu đại dương là một trong những vấn đề thách thức nhất trong nghiên cứu biến chất UHP, điều này rất quan trọng cho việc hiểu cơ chế địa động lực của Trái Đất rắn. Như một người du hành bị hụt nén vào độ sâu manti và sau đó được nâng lên bề mặt, các đới biến chất UHP kiểu đại dương chứng kiến quá trình từ hụt nén đến khai thác và là mục tiêu lý tưởng để nghiên cứu hành vi địa hóa và chu trình của các nguyên tố trong các vùng hụt nén. Sự phát triển kiến tạo của một vành đai orogen hội tụ thường được chia thành hai giai đoạn: hụt nén đại dương và theo sau là sự hụt nén và va chạm lục địa, và hai ví dụ tiêu biểu nhất của các vành đai orogen là Alpes và Himalaya. Do đó, nghiên cứu về đới biến chất UHP kiểu đại dương là biên giới của lý thuyết kiến tạo mảng hiện tại.
Từ khóa
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