Kinematic modelling of the West Antarctic Rift system, Ross Sea, Antarctica

Author(s): Busetti, Martina; Spadini, Giacomo; van der Wateren, Frederik M.; Cloetingh, Sierd A. P. L.; Zanolla, Claudio
Author Affiliation(s): Primary:
Osservatorio Geofisico Sperimentale, Trieste, Italy
Other:
Vrije Universiteit, Amsterdam, Netherlands
Volume Title: Lithosphere dynamics and environmental change of the Cenozoic West Antarctic Rift system
Volume Author(s): van der Wateren, Frederik M., editor; Cloetingh, Sierd A. P. L.
Source: Lithosphere dynamics and environmental change of the Cenozoic West Antarctic Rift system, edited by Frederik M. van der Wateren and Sierd A. P. L. Cloetingh. Global and Planetary Change, 23(1-4), p.79-103. Publisher: Elsevier, Amsterdam, Netherlands. ISSN: 0921-8181
Note: In English. 93 refs.; illus., incl. sects., 3 tables, geol. sketch map
Summary: In this study, we investigate the thermo-mechanical controls on the formation of the Ross Sea basin (Antarctica) and the uplift of the adjacent Transantarctic Mountains (TAM) rift shoulder, which started in the Late Cretaceous and continued until the present time. Quantitative forward modelling has been performed along three 700 to 800 km long East-West offshore profiles, extended inland to the front of the TAM. The modelling is constrained by an extensive database of multichannel seismic (MCS), refraction seismic, Ocean Bottom Seismographs (OBS), and gravity data. MCS data is tied to well stratigraphy from DSDP leg 28, CIROS-1 and MSTSS-1. Quantitative estimates of uplift of the TAM are provided by previous work on apatite fission track analysis. We incorporate the finite strength of the lithosphere in basin formation models using the concept of the level of necking. Lateral variations of necking level and associated bulk rheological properties (with necking levels ranging from 15 km in the northernmost, to 20 km in the central and 23 km to the southernmost profiles) are required to explain the observed crustal geometries. High values of effective elastic thickness (more than 30 km) and pre-rift lithospheric thicknesses (220-230 km), indicating a cold lithosphere in a pre-rift cratonic setting, are consistent with elevation of the rift shoulder. The western parts of the profiles appear to have unusually high stretching values without the development of oceanic crust. Inferred average values of stretching factors vary from 2.3 to 2.8, equivalent with extension in the Ross Sea of 115% to 140%. The modelling result for the uplift of the TAM predicts a late Cretaceous tectonic uplift of about 1.5 to 2.0 km, and a Cenozoic uplift of about 1.3 km restricted to southern Victoria Land. Abstract Copyright (1999) Elsevier, B.V.
Year of Publication: 1999
Research Program: DSDP Deep Sea Drilling Project
Key Words: 18 Geophysics, Solid-Earth; Antarctic Ocean; Antarctica; Crust; Data processing; Digital simulation; Elasticity; Extension; Geophysical methods; Geophysical profiles; Geophysical surveys; Gravity anomalies; Gravity methods; Kinematics; Lithosphere; Models; Numerical models; Ocean bottom seismographs; Plate tectonics; Refraction methods; Rift zones; Rifting; Ross Sea; Seismic methods; Seismic profiles; Seismographs; Southern Ocean; Strength; Surveys; Thermomechanical properties; Thickness; Transantarctic Mountains; Two-dimensional models; Uplifts; Victoria Land; West Antarctic Rift; West Antarctica
Record ID: 2000025973
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from CAPCAS, Elsevier Scientific Publishers, Amsterdam, Netherlands

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