DEEP STRUCTURE OF PENTADAKTYLOS AND MESAORIA RANGE IN CYPRUS

被引：10

作者：

AUBERT, M

BAROZ, F

机构：

[1] INST PHYS GLOBE PARIS, LAB PETROL, CLERMONT FERRAND, FRANCE

[2] UNIV NANCY 1, NANCY, FRANCE

来源：

REVUE DE L INSTITUT FRANCAIS DU PETROLE | 1974年 / 29卷 / 03期

关键词：

D O I：

10.2516/ogst:1974016

中图分类号：

TE [石油、天然气工业]; TK [能源与动力工程];

学科分类号：

0807 ; 0820 ;

摘要：

引用

页码：361 / 373

页数：13

共 16 条

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[2]

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[3]

BAROZ F, 1974, REV I FRANC PETROLE, V29, P3

[4]

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[6] THE GEOLOGY AND GRAVITY ANOMALIES OF THE TROODOS MASSIF, CYPRUS [J].

GASS, IG ;

MASSONSMITH, D .

PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL AND PHYSICAL SCIENCES, 1963, 255 (1060) :417-467

[7]

LAPIERRE H, 1968, CR ACAD SCI D NAT, V266, P1817

[8]

Mantis M., 1971, KYPRIAKOS LOGOS, V3, P202

[9] SEISMIC VELOCITIES AT CYPRUS OUTCROP [J].

MATTHEWS, DH ;

LORT, J ;

VERTUE, T ;

POSTER, CK ;

GASS, IG .

NATURE-PHYSICAL SCIENCE, 1971, 231 (26) :200-&

[10] TROODOS OPHIOLITIC COMPLEX WAS PROBABLY FORMED IN AN ISLAND ARC [J].

MIYASHIRO, A .

EARTH AND PLANETARY SCIENCE LETTERS, 1973, 19 (02) :218-224

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