A POSSIBLE MECHANISM FOR EPEIROGENIC UPLIFT

[1] [Anonymous], 1877, GEOL MAG, DOI DOI 10.1017/S0016756800151465

[2] A SEISMIC REFRACTION AND REFLECTION STUDY OF THE CONTINENT-OCEAN TRANSITION BENEATH THE NORTH BISCAY MARGIN [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1982, 305 (1489): : 5 - 25

[3] BALLY AW, 1982, PHIL T R SOC A, V305, P41

[4] ON THE EVOLUTION OF RIFTED CONTINENTAL MARGINS - COMPARISON OF MODELS AND OBSERVATIONS FOR THE NOVA-SCOTIAN MARGIN [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1982, 70 (03): : 667 - 715

[5] CONTINENTAL ACCRETION - FROM OCEANIC PLATEAUS TO ALLOCHTHONOUS TERRANES [J]. SCIENCE, 1981, 213 (4503) : 47 - 54

[6] THE MAGNETIC QUIET ZONE IN THE EASTERN GULF OF ADEN - IMPLICATIONS FOR THE EARLY DEVELOPMENT OF THE CONTINENTAL-MARGIN [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1982, 68 (01): : 171 - 201

[7] A MODEL FOR FLOOD BASALT VULCANISM [J]. JOURNAL OF PETROLOGY, 1980, 21 (04) : 629 - 650

[8] PETROGENESIS OF VOLCANIC ROCKS OF CENTRAL NORTH ISLAND NEW ZELAAND AS INDICATED BY A STUDY OF SR87/SR86 RATIOS AND SR RB K U AND TH ABUNDADANCES [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1968, 32 (07) : 699 - &

[9] PETROGENESIS OF THE TERTIARY ANOROGENIC VOLCANIC SERIES OF SOUTHERN QUEENSLAND, AUSTRALIA, IN THE LIGHT OF TRACE-ELEMENT GEOCHEMISTRY AND O, SR AND PB ISOTOPES [J]. JOURNAL OF PETROLOGY, 1982, 23 (03) : 344 - 382

[10] THE OCEAN-CONTINENT TRANSITION IN THE UNIFORM LITHOSPHERIC STRETCHING MODEL - ROLE OF PARTIAL MELTING IN THE MANTLE [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1982, 305 (1489): : 27 - 43

[1] [Anonymous], 1877, GEOL MAG, DOI DOI 10.1017/S0016756800151465

[2] A SEISMIC REFRACTION AND REFLECTION STUDY OF THE CONTINENT-OCEAN TRANSITION BENEATH THE NORTH BISCAY MARGIN [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1982, 305 (1489): : 5 - 25

[3] BALLY AW, 1982, PHIL T R SOC A, V305, P41

[4] ON THE EVOLUTION OF RIFTED CONTINENTAL MARGINS - COMPARISON OF MODELS AND OBSERVATIONS FOR THE NOVA-SCOTIAN MARGIN [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1982, 70 (03): : 667 - 715

[5] CONTINENTAL ACCRETION - FROM OCEANIC PLATEAUS TO ALLOCHTHONOUS TERRANES [J]. SCIENCE, 1981, 213 (4503) : 47 - 54

[6] THE MAGNETIC QUIET ZONE IN THE EASTERN GULF OF ADEN - IMPLICATIONS FOR THE EARLY DEVELOPMENT OF THE CONTINENTAL-MARGIN [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1982, 68 (01): : 171 - 201

[7] A MODEL FOR FLOOD BASALT VULCANISM [J]. JOURNAL OF PETROLOGY, 1980, 21 (04) : 629 - 650

[8] PETROGENESIS OF VOLCANIC ROCKS OF CENTRAL NORTH ISLAND NEW ZELAAND AS INDICATED BY A STUDY OF SR87/SR86 RATIOS AND SR RB K U AND TH ABUNDADANCES [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1968, 32 (07) : 699 - &

[9] PETROGENESIS OF THE TERTIARY ANOROGENIC VOLCANIC SERIES OF SOUTHERN QUEENSLAND, AUSTRALIA, IN THE LIGHT OF TRACE-ELEMENT GEOCHEMISTRY AND O, SR AND PB ISOTOPES [J]. JOURNAL OF PETROLOGY, 1982, 23 (03) : 344 - 382

[10] THE OCEAN-CONTINENT TRANSITION IN THE UNIFORM LITHOSPHERIC STRETCHING MODEL - ROLE OF PARTIAL MELTING IN THE MANTLE [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1982, 305 (1489): : 27 - 43