MULTICHANNEL SEISMIC DATA IMAGING OF INVERSION TECTONICS OF THE ALBORAN RIDGE (WESTERN MEDITERRANEAN-SEA)

被引：65

作者：

BOURGOIS, J

MAUFFRET, A

AMMAR, A

DEMNATI, A

机构：

[1] UNIV MOHAMMED 5,DEPT SCI TERRE,RABAT,MOROCCO

[2] OFF NATL RECH & EXPLOITAT PETROLIERES,RABAT,MOROCCO

来源：

GEO-MARINE LETTERS | 1992年 / 12卷 / 2-3期

关键词：

D O I：

10.1007/BF02084921

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The Alboran Ridge is an anticlinorium structure trending N65-degrees-E bounded by two main right lateral strike-slip fault systems, one north and one south. These transpressional features connect westward to a pull-apart zone where massive diapirism occurs. The orientation of the diapiric zone is N150-degrees-E. That orientation and the right lateral motion along the Alboran Ridge fit a N150-degrees-E convergent motion between African and Iberian plates. We suggest that the southern Alboran Basin evolved as an extensional stage from Burdigalian to Langhian and as a transpressional stage during Tortonian to present time.

引用

页码：117 / 122

页数：6

共 33 条

[21] STRESS PATTERNS AND KINEMATICS OF THE RIFIAN BELT (MOROCCO) FROM TORTONIAN TO PRESENT [J].

MOREL, JL .

GEODINAMICA ACTA, 1989, 3 (04) :283-294

[22]

Morelli C., 1971, B GEOFIS TEOR APPL, V13, P99

[23]

OLDOW JS, 1990, GEOLOGY, V18, P991, DOI 10.1130/0091-7613(1990)018<0991:TOFALB>2.3.CO

[24]

[25]

Olivet J.L., 1973, B SOC GEOL FRANCE, VXV, P108

[26]

Olivet JL, 1973, INITIAL REPORTS DEEP, V13, P1417

[27]

PASTOURET L, 1975, B SOC GEOLOGIQUE FRA, V17, P1168

[28]

PHILIP H, 1987, ANN GEOPHYS B-TERR P, V5, P301

[29]

PLATT JP, 1989, GEOLOGY, V17, P540, DOI 10.1130/0091-7613(1989)017<0540:ECOTCL>2.3.CO

[30]

← 1 2 3 4 →