Low-angle faults above and below a blueschist belt-Tinos Island, Cyclades, Greece

被引：140

作者：

Avigad, Dov ^{[1
]}

Garfunkel, Zvi ^{[1
]}

机构：

[1] Hebrew Univ Jerusalem, Inst Earth Sci, Dept Geol, IL-91904 Jerusalem, Israel

来源：

TERRA NOVA | 1989年 / 1卷 / 02期

关键词：

D O I：

10.1111/j.1365-3121.1989.tb00350.x

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

New observations from the Island of Tinos, Greece, allow a better definition of the structural position of the Alpine (Eocene) blueschist belt exposed in the islands of the Aegean Sea. These blueschists, over a significant part of the Aegean sea, are delimited from below by a low-angle thrust fault, while from above they are delimited by a low-angle, normal-type fault which omits a substantial crustal interval. Both underlying and overlying rocks were not affected by the high? metamorphism. The rapid uplift and exhumation of the high? rocks was therefore mainly the result of fault movements rather than erosion and whole-crust uplifting. The low-angle normal fault apparently had a major role in the uplift of the blueschists.

引用

页码：182 / 187

页数：6

共 26 条

[11]

Durr S., 1978, ALPS APENNINES HELLE, V38, P455

[12]

England P.C., 1977, J GEOLOGICAL SOC LON, V134, P201, DOI [10.1144/gsjgs.134.2.0201, DOI 10.1144/GSJGS.134.2.0201]

[13]

Godfriaux I., 1977, B GEOL SOC FR, V19, P45

[14] ISOTOPIC DATING OF PRE-ALPIDIC ROCKS FROM THE ISLAND OF IOS (CYCLADES, GREECE) [J].

HENJESKUNST, F ;

KREUZER, H .

CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1982, 80 (03) :245-253

[15]

JACOBSHAGEN V, 1976, Z DTSCH GEOL GES, V127, P337

[16]

Katsikatsos G, 1977, P 6 C GEOL AEG REG A, V1, P211

[17]

MALUSKI H, 1987, B SOC GEOL FR, V3, P833

[18]

Papanikolaou D. J, 1987, CHEM TRANSPORT METAS, P429, DOI [DOI 10.1007/978-94-009-4013-0_16, 10.1007/978-94-009-4013-0_16]

[19]

Papanikolaou D.J., 1979, B SOC GEOL FRANCE, P21

[20]

Papanikolau D, 1984, GEOL SOC LOND SPEC P, V17, P551, DOI DOI 10.1144/GSL.SP.1984.017.01.42

← 1 2 3 →