... the inner belt to the outer belt of the active area of the Emei mantle plume, and the dolomitization was not strictly controlled by faults (Fig.  5 ). Fig. 5. Thickness map of the middle Permian dolomitized rocks in East Yunnan overlain by the upper Permian fault patterns (Luo et al. 1988 , 2012...

... of the Ginsburg MV and its reference core. outer ring faults is visible in seismic reflection profiles (see Initial Reports of the Ocean Drilling Program Leg 160; Emeis et al., 1996). The cores recovered from the two MVs consist of mud breccia, with no or thin hemipelagic deposits at the top (Fig. 2). The draping...

... in the rift between metamorphic highlands to the east and west. Magadi Trachyte (ca. 1.4–0.8 Ma) covers much of the rift floor, cut by rift-parallel faulting. Pliocene-Pleistocene volcanos are found throughout the region, mostly trachyandesitic to basaltic with a few carbonatites ( Baker and Mitchell, 1976...

... of turbidites and high-angle extensional faults have been observed and the construction of the magnetostratigraphic record was hindered by overprints that could not be removed ( E meis et alii , 1996 ). A total of 59 sapropel layers are present in the composite section of Site 964 ( S akamoto et alii , 1998...

... is an elongated, intramontane basin located between the Central and Eastern cordilleras ( Figures 1 , 2 ). The UMV is limited to the west by the westward-dipping Girardot and Chusma fault systems that separate the UMV from the crystalline rocks of the Central Cordillera. The invasion of the Cretaceous sea...

...) Schematic tectonic map of the central-eastern Gangdese tectono-magmatic belt of the southern Lhasa terrane (modified from Yin et al., 1994 ; Kapp et al., 2007 ; Ma et al., 2017a ), showing the Gangdese décollement, which is located to the south of the retro-arc fold-thrust belts (Emei La–Gulu-Hamu thrust...

...Trevor Burchette; Gavrielle Groves-Gidney; Kul Karcz Abstract Interpretation of seismic data over the southeastern flank of the Eratosthenes High shows nine principal seismic stratigraphic units overlying probable faulted basement. Among these are three superposed carbonate platforms that build...

..., and its reactivation periods, near the Tailai gas field; and (4) characterize fault-related hydrocarbon accumulation processes in hydrothermal dolomite reservoirs. The REEY analyses were completed using laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) at Wuhan SampleSolution...

... history is not considered here). Pleistocene compression or transpression is locally documented by faults that cut Pliocene sediments ( McCay & Robertson 2012 b ). In addition, a small number of transverse fault planes within the Kyrenia Range are mantled by relatively immature scree talus...

... by Murphy et al. (1997) , our conclusions are probably compatible with their geologic observations in southern Tibet on and to the south of this study area. According to the geometric relationships between thrust faults and magmatic rocks in Figure 2 of Murphy et al., the Emei La thrust system must have...

... fraction is made of turbiditic sands, and a finer fraction is composed of hemipelagic clays ( Ryan et al., 1973 ; Hsu et al., 1978 ; Emeis et al., 1996 ). The Nile deep-sea fan is the largest sedimentary clastic accumulation within the Mediterranean Sea, and it lies in a complex geodynamic setting...

... Permian Emei taphrogeny gradually reached a peak ( Z. Luo et al., 1988 ), leading to the massive eruption of basalts along the nearly east-west–trending basement fault belt and associated secondary faults ( C. Zhu et al., 2010 ). This event is thought to have been an important source of Permian...

... the Late Eocene. The termination of subduction during continental collision may have permitted thermal relaxation Fig. 11. Geological sketch map of the northeastern margin of the Tenda Massif showing the presence of en echelon folds in allochthonous units adjacent to a sinistral wrench fault. Legend: la...

... topographical loading is absent, gliding may dominate, leading to the formation of predominantly margin-parallel normal faults and small diapirs (e.g. rollers) in proximal areas, and margin-parallel folds and thrusts further downdip (e.g. Cobbold & Szatmari 1991 ; Vendeville 2005 ; Loncke et al. 2006...

... taphrogenesis (rifting) from the late Neoproterozoic to early Cambrian. The central Sichuan paleo-uplift was undergoing ENE extension, and preexisting ESE- and nearly E-W–striking faults were oblique to the ENE principal stress orientation. This led to a local stress field favoring dextral shear near fault...

... measurements were conducted on a slab collected at the surface of the archive half core. The slabs were then regularly sampled to obtain isotopic data. * Corresponding author: e-mail: [email protected] La dégradation de la matière organique est le moteur de l'évolution biogéochimique des...