Magma-poor rifted margins are being increasingly recognized in present-day Atlantic-type
systems. However, findings of fossil areas floored by exhumed mantle or hyper-extended …

This work aims to review and discuss with new interpretations the tectonic evolution of the
Ivrea Verbano Zone (IVZ), to highlight how inheritance from previous orogenic cycles may …

Rifted margins are the result of the successful process of thinning and breakup of the
continental lithosphere leading to the formation of new oceanic lithosphere. Observations on …

Rifted margins are commonly defined as magma-poor or magma-rich archetypes based on
their morphology. We re-examine the prevailing model inferred from this classification that …

We summarize here observations from the South Atlantic Angola–Gabon rifted margin. Our
study was based on the interpretation of a selection of deep penetration depth-migrated …

Abstract Interpretation of long‐offset 2D depth‐imaged seismic data suggests that outer
continental margins collapse and tilt basinward rapidly as rifting yields to seafloor spreading …

From the apex of the NW Sub-basin of the South China Sea, we present new long-cable
deep-penetration seismic profiles and deepwater drillings together with corrected seismic …

Although it is generally accepted that many distal, magma-poor rifted margins are
asymmetric and can be divided into lower and upper plate margins, little is known about the …

Tectonic inheritance deals with the influence of pre-existing or pre-rift elements on the
geometry, genesis and propagation of rift-related faults. Inheritance strongly controls the …

南海北部陆缘发育独特的远端带结构, 以“裂谷宽, 基底厚和地貌起伏” 为主要特点,
显著有别于经典贫岩浆型和富岩浆型张裂陆缘. 为了解释陆缘结构的成因, 综合已有研究进展和 …