摘要[意义] 细粒沉积岩纹层是半深湖—深湖盆内地层中可分辨的, 最基本的沉积单元结构,
单层厚度一般小于10 mm, 其物质组分, 连续性和几何形态对于恢复古环境变迁和沉积模式具有 …

The Aptian evaporitic transitional sequence (sag phase) of the Brazilian marginal basins
records the first connection between the Central and South Atlantic oceans in the equatorial …

Mapping and luminescence aging of raised marine terraces and aeolian ridges along an∼
90 km coastal stretch in southwestern Sicily provide the first quantitative assessment of …

Paleoceanographic information from submarine overflows in the vicinity of oceanic
gateways is of major importance for resolving the role of ocean circulation in modulating …

Interbedded contourites, turbidites and pelagites are commonplace in many deep‐water
slope environments. However, the distinction between these different facies remains a …

Abstract The Central Uplift region of the Tarim Basin contains a series of thick Ordovician
carbonates that form fractured-vuggy hydrocarbon-rich reservoirs along an unconformity …

The present research explores a diverse suite of soft sediment deformation structures
(SSDS) combined with clastic dykes and shear deformation bands distributed throughout a …

Sea-floor fans containing both carbonate and siliciclastic detritus are rarely recognized in
the rock record but are common within the Permian upper Wolfcamp Formation in the …

The Miocene, syn-rift mixed siliciclastic-carbonate strata has been a long sought-after
reservoir objective in the Red Sea rift basins. Despite being viable prospects, their …

Mixed deposits are sediments consisting of external clastic (epiclastic or terrigenous),
intrabasinal components and pyroclastic components. The mixture, comprising variable …