Results 161 to 170 of about 68,988 (223)
An integrated petrophysical and rock physics characterization of the Mangahewa Formation in the Pohokura field, Taranaki Basin. [PDF]
Sci RepHossain S, Rahman N.
europepmc +1 more source
Elemental logging evidence for paleoenvironmental reconstruction of the ordovician strata in the Western Ordos basin, China. [PDF]
Sci RepZhao Z +6 more
europepmc +1 more source
Some of the next articles are maybe not open access.
Related searches:
Related searches:
Skagerrak Graben—the offshore continuation of the Oslo Graben
Tectonophysics, 1990Abstract New seismic mapping of Skagerrak reveals eight structural provinces. In particular, the Skagerrak Graben appears to be the continuation of the Oslo Graben. The Skagerrak Graben is defined by two major Late Paleozoic faults trending northeast-southwest connecting with the faults bounding the Oslo Graben.
H.E. Ro +3 more
openaire +1 more source
2010
A continental graben structure or rift is a narrow, elongated, fault-bounded structure in the Earth’s crust (Fig. 3.1). Grabens consist of a central axial depression flanked by steep walls and elevated shoulders that plunge steeply into the rift axis and slope gradually towards the exterior (Fig. 3.2).
Wolfgang Frisch +2 more
openaire +1 more source
A continental graben structure or rift is a narrow, elongated, fault-bounded structure in the Earth’s crust (Fig. 3.1). Grabens consist of a central axial depression flanked by steep walls and elevated shoulders that plunge steeply into the rift axis and slope gradually towards the exterior (Fig. 3.2).
Wolfgang Frisch +2 more
openaire +1 more source
Tectonophysics, 1987
Abstract Deep basins on continental crust can be divided into two main types: basins with normal faults and the basement both tilted in the same direction (S-type) and in opposite directions (A-type). A high intensity of stretching occurs in the basins of the A-type under a large angle of block tilting.
openaire +1 more source
Abstract Deep basins on continental crust can be divided into two main types: basins with normal faults and the basement both tilted in the same direction (S-type) and in opposite directions (A-type). A high intensity of stretching occurs in the basins of the A-type under a large angle of block tilting.
openaire +1 more source