Formation of hydrocarbon reservoirs in the deep Earth's crust, with the periodic axial plunge of the rift floor during the extension of the Earth's
crust, and with the elevation
Origin of continental crust; the downsliding and assimilation of basaltic oceanic
crust do not account for the bulk of the
continental granitic
Formation of hydrocarbon reservoirs in the deep Earth's crust, with the periodic axial plunge of the rift floor during the extension of the Earth's
crust, and with the elevation
Oxygen isotopic alteration rate of continental crust recorded by detrital zircon and its implication for deep-time weatheringLi, Gaojun,
Yang, Ruiyu,
Xu, Zhewen,
Hartmann, Jens,
Hedding, David W.,
Li, Xianhua,
Ernst, Richard E.,
Li, Zhong-Hai,
Zou, Hao,
Li, Zhongquan,
Chen, Jun crystallization. A new algorithm is introduced to reconstruct the average O alteration rate of
continental crust