So sánh phương pháp

	Phân tích sự lún lòng chậu	Phân tích Cổ từ trường
Lĩnh vực	Khoa học Trái Đất	Khoa học Trái Đất
Họ	Process / pipeline	Process / pipeline
Năm ra đời	1978	1906
Người khởi xướng	McKenzie and Sclater	Bernard Brunhes and Motonori Matuyama
Loại	tectono-sedimentary analysis pipeline	temporal constraint pipeline
Công trình gốc	Sclater, J. G., & Christie, P. A. F. (1980). Continental stretching: An explanation of the post-mid-Cretaceous subsidence of the Central North Sea Basin. Journal of Geophysical Research, 85(B7), 3711–3739.	Butler, R. F. (1992). Paleomagnetism: Magnetic Domains to Geologic Terranes. Blackwell Scientific Publications.
Tên gọi khác	tectonic subsidence, backstripping, thermal history analysis	paleomagnetic dating, magnetostratigraphy, paleomagnetic remanence
Liên quan	4	3
Tóm tắt	Basin subsidence analysis is the quantitative study of how sedimentary basins deepen over geological time, driven by tectonics, isostasy, and load. Formalized by McKenzie (1978) and Sclater and Christie (1980), this method reveals the mechanical causes of basin development, predicts subsurface temperature and pressure histories, and constrains petroleum generation. Analysis integrates well stratigraphy, seismic geometry, gravity data, and thermal models to reconstruct basin evolution.	Paleomagnetism analysis is the study of ancient magnetic properties of rocks, measuring fossil magnetization to determine paleomagnetic field history and assign geological ages. Pioneered by Brunhes (1906) and systematized by Tauxe (2010), this method reveals geomagnetic reversals, polar wander paths, and paleomagnetic chronology independent of fossil biostratigraphy. Analysis integrates laboratory rock magnetism with field sampling to build high-resolution timescales and constrain plate motion.