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Tuổi U-Pb zircon, đặc điểm địa hóa và thành phần đồng vị Sr-Nd-Hf của granitoid Neoproterozoic ở rìa tây bắc của khối Yangtze (Nam Trung Quốc): Những hệ quả cho sự tiến hóa kiến tạo Neoproterozoic
Tóm tắt
Sự xuất hiện rộng rãi của magmatism Neoproterozoic dọc theo khối Yangtze mang lại thông tin quan trọng để hiểu biết về sự tiến hóa Neoproterozoic của khối này. Tại rìa tây bắc của khối Yangtze, phức hợp xâm nhập Hannan (汉南) bao gồm các granitoid Wudumen (五堵门), Erliba (二里坝) và Zushidian (祖师殿). Bằng phương pháp xác định tuổi zircon U-Pb LA-ICP-MS, các granitoid Wudumen và Erliba thu được tuổi kết tinh magma lần lượt là 785±4 và 778±3 triệu năm. Mẫu từ ba granitoid này cho thấy hàm lượng SiO2 biến đổi từ 58.8% đến 72.6%. Chúng được đặc trưng bởi sự phong phú của Al2O3 (14.97%–17.87%), Na2O (3.80%–5.33%) và Sr (504 ppm–741 ppm), và thiếu hụt Y (<19 ppm) và HREE (ví dụ, Yb<1.6 ppm), dẫn đến tỷ lệ Sr/Y (29–161) và (La/Yb)N (7.3–27.8) cao. Các đặc điểm địa hóa của các granitoid này tương đồng với adakite. Các granitoid có giá trị zircon ɛHf(t) từ +3.65 đến +10.05, giá trị toàn bộ đá ɛNd(t) từ −0.09 đến +2.98 và tỷ lệ 87Sr/86Sr ban đầu toàn bộ đá từ 0.703 4 đến 0.703 9, cho thấy magma của chúng bắt nguồn từ một nguồn vỏ địa sinh trẻ. Cùng với các thành phần địa hóa và đồng vị Hf-Sr-Nd, có thể cho rằng các granitoid hình thành trong môi trường cung đảo và bắt nguồn từ sự nấu chảy một phần của một phiến đại dương bị chìm. Các kết quả này hỗ trợ mô hình rằng khối Yangtze được bao quanh bởi đại dương và magmatism cung đảo ở các rìa phía bắc và tây bắc của nó trong thời kỳ Neoproterozoic.
Từ khóa
#neoproterozoic; granitoids; U-Pb zircon dating; geochemical characteristics; Sr-Nd-Hf isotopes; Yangtze blockTài liệu tham khảo
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