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Titolo:
MESOZOIC ANOMALIES IN THE BAY OF BENGAL
Autore:
RAMANA MV; NAIR RR; SARMA KVLNS; RAMPRASAD T; KRISHNA KS; SUBRAHMANYAM V; DCRUZ M; SUBRAHMANYAM C; PAUL J; SUBRAHMANYAM AS; CHANDRASEKHAR DV;
Indirizzi:
NATL INST OCEANOG PANAJI 403004 GOA INDIA NATL GEOPHYS RES INST HYDERABAD 500007 ANDHRA PRADESH INDIA NATL INST OCEANOG,REG CTR VISAKHAPATNAM 530023 INDIA
Titolo Testata:
Earth and planetary science letters
fascicolo: 3-4, volume: 121, anno: 1994,
pagine: 469 - 475
SICI:
0012-821X(1994)121:3-4<469:MAITBO>2.0.ZU;2-T
Fonte:
ISI
Lingua:
ENG
Soggetto:
EASTERN INDIAN-OCEAN; GONDWANALAND; BREAKUP; EVOLUTION; AUSTRALIA; RECONSTRUCTION; CONTINENTS; ANTARCTICA;
Tipo documento:
Article
Natura:
Periodico
Settore Disciplinare:
Science Citation Index Expanded
Citazioni:
33
Recensione:
Indirizzi per estratti:
Citazione:
M.V. Ramana et al., "MESOZOIC ANOMALIES IN THE BAY OF BENGAL", Earth and planetary science letters, 121(3-4), 1994, pp. 469-475

Abstract

The analysis of 8200 line km of total magnetic intensity data in the Bay of Bengal, northeastern Indian Ocean, revealed the presence of approximately N30-degrees-E-trending seafloor spreading type magnetic anomalies. These anomalies resemble the Mesozoic anomaly series (M11-M0) reported elsewhere. The oldest anomaly (M11, 132.5 Ma) identified close to the east coast of India is followed by the younger series of Mesozoic anomalies towards the offshore. Some of the anomalies are offset by 60-80 km. The configuration of the offsets of the isochrons allowedus to propose approximately N120-degrees-E-trending oceanic fracture zones. The Mesozoic crust of 132.5-118 Ma is estimated to evolve with an average half-spreading rate of 3.5 cm/yr, except for the ocean floor between the M9 and M4 magnetic isochrons. This part of the crust appears to be affected by the buried subsurface 85-degrees-E Ridge.

ASDD Area Sistemi Dipartimentali e Documentali, Università di Bologna, Catalogo delle riviste ed altri periodici
Documento generato il 14/08/20 alle ore 04:59:13