(Table 1) Age of Cretaceous seamounts in the Western Pacific

• Main Author: Stepashko, A A
• Format: Dataset
• Language: English
• Published: PANGAEA 2006
• Subjects: Age; 40Ar/39Ar Argon-Argon; dated; dated standard deviation; Archive of Ocean Data; ARCOD; Calculated; Cross; Daiichi-Kashima; Event label; Golden_Dragon; H11; Haydn; Isakov; Kapsitotwa; Khatchaturian; Latitude of event; Liszt; Lo-En; Longitude of event; Magata; Mahler; Makarov; Mendelssohn-E; Mendelssohn-W; Miami_smt; Mij-Lep_(Heezen); Paumakaua; Rachmaninov; Schumann-W; Scripps; Takuyo-Daisan; Wageman; West Pacific; Wilde; Winterer; Okhotsk; Pacific; Schumann; Chukchi; Chukchi Peninsula
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.749840; https://doi.org/10.1594/PANGAEA.749840

Dynamics of the Pacific Plate is recorded in the systematic variation of location and the 40Ar-39Ar age of seamounts in the Western Pacific from 120 to 65 Ma ago. The seamounts are grouped into three linear zones as long as 5000 km. The seamounts become younger in the southeastern direction along the strike of these zones. Correlation between age and location of seamounts allows to divide the history of their formation into three stages. Rate of seamount growth was relatively low (2-4 cm/yr) during the first and the third stages within intervals of 120-90 and 85-65 Ma, whereas during the second stage (90-85 Ma), the seamounts were growing very fast (80-100 cm/yr). In the midst of this stage, at ~87 Ma ago, magmatic activity increased abruptly. Dynamics of seamount building is in good agreement with (1) pulses in development of the Ontong Java, Manihiki, and Caribbean-Colombian oceanic plateaus; (2) age of spreading acceleration in the mid-Cretaceous; and (3) a short period when the Izanagi Plate ceased to exist and the Kula Plate was formed. Variation in seamounts' age and location are in consistence with the hypothesis of diffuse extension of the Pacific Plate in course of its motion with formation of impaired zones of decompression melting. Direction of extension (325°-340° NW) calculated from the strike of seamount zones is consistent with the path of the Pacific Plate (330° NW) in the Late Cretaceous. Immense perioceanic volcanic belts were formed at that time along the margin of the Asian continent. The Okhotsk-Chukchi Peninsula Belt extends at a right angle to the compression vector. Three stages of this belt's evolution are synchronous with the stages of seamount formation in the Pacific Plate. Delay in origination of the East Sikhote-Alin Volcanic Belt and its different orientation were caused by counterclockwise rotation of the vector of convergence of oceanic and continental plates in the mid-Cretaceous. At the same time, i.e. 95-85 Ma ago, volcanic activity embraced the entire continental margin and ...