DETRITAL MODE EVOLUTION OF THE RIFTED CONTINENTAL-MARGIN LONGOBUCCO SEQUENCE (JURASSIC), CALABRIAN ARC, ITALY

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作者：

ZUFFA, GG

GAUDIO, W

ROVITO, S

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JOURNAL OF SEDIMENTARY PETROLOGY | 1980年 / 50卷 / 01期

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P5 [地质学];

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0709 ; 081803 ;

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页码：51 / 61

页数：11

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[1] SUBSIDENCE AND SEDIMENTATION ON JURASSIC PASSIVE CONTINENTAL-MARGIN, SOUTHERN ALPS, ITALY
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[7] EARLY CRETACEOUS INTRAARC DUCTILE STRAIN IN TRIASSIC-JURASSIC AND CRETACEOUS CONTINENTAL-MARGIN ARC ROCKS, PENINSULAR RANGES, CALIFORNIA
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[8] ON THE FORMATION AND EVOLUTION OF THE MESOZOIC-CENOZOIC ACTIVE CONTINENTAL-MARGIN AND ISLAND-ARC TECTONICS OF THE WESTERN PACIFIC-OCEAN
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[10] DETRITAL ZIRCON GEOCHRONOLOGY OF UPPER PROTEROZOIC TO LOWER PALEOZOIC CONTINENTAL-MARGIN STRATA OF THE KOOTENAY ARC - IMPLICATIONS FOR THE EARLY PALEOZOIC TECTONIC DEVELOPMENT OF THE EASTERN CANADIAN CORDILLERA
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