Tectonic implications of fault-scarp–derived volcaniclastic deposits on Macquarie Island: Sedimentation at a fossil ridge-transform intersection?

2005 ◽  
Vol 117 (1) ◽  
pp. 18 ◽  
Author(s):  
Nathan R. Daczko ◽  
Sharon Mosher ◽  
Millard F. Coffin ◽  
Timothy A. Meckel
Keyword(s):  
Fault Scarp ◽  
Macquarie Island ◽  
Tectonic Implications ◽  
Volcaniclastic Deposits

Is Efate (Vanuatu, SW Pacific) a result of subaerial or submarine eruption? An alternative model for the 1 Ma Efate Pumice Formation

2010 ◽  
Vol 2 (3) ◽  
Author(s):  
Robert Stewart ◽  
Karoly Németh ◽  
Shane Cronin
Keyword(s):  
Fault Scarp ◽  
Pyroclastic Rock ◽  
Shallow Marine ◽  
The North ◽  
Sw Pacific ◽  
Volcanic Succession ◽  
Volcaniclastic Deposits ◽  
Caldera Subsidence ◽  
Volcaniclastic Succession ◽  
Explosive Event

AbstractThe Efate Pumice Formation (EPF) is a trachydacitic volcaniclastic succession widespread in the central part of Efate Island and also present on Hat and Lelepa islands to the north. The volcanic succession has been inferred to result from a major, entirely subaqueous explosive event north of Efate Island. The accumulated pumice-rich units were previously interpreted to be subaqueous pyroclastic density current deposits on the basis of their bedding, componentry and stratigraphic characteristics. Here we suggest an alternative eruptive scenario for this widespread succession. The major part of the EPF is distributed in central Efate, where pumiceous pyroclastic rock units several hundred meters thick are found within fault scarp cliffs elevated about 800 m above sea level. The basal 200 m of the pumiceous succession is composed of massive to weakly bedded pumiceous lapilli units, each 2-3 m thick. This succession is interbedded with wavy, undulatory and dune bedded pumiceous ash and fine lapilli units with characteristics of co-ignimbrite surges and ground surges. The presence of the surge beds implies that the intervening units comprise a subaerial ignimbrite-dominated succession. There are no sedimentary indicators in the basal units examined that are consistent with water-supported transportation and/or deposition. The subaerial ignimbrite sequence of the EPF is overlain by a shallow marine volcaniclastic Rentanbau Tuffs. The EPF is topped by reef limestone, which presumably preserved the underlying EPF from erosion. We here propose that the EPF was formed by a combination of initial subaerial ignimbrite-forming eruptions, followed by caldera subsidence. The upper volcaniclastic successions in our model represent intra-caldera pumiceous volcaniclastic deposits accumulated in a shallow marine environment in the resultant caldera. The present day elevated position of the succession is a result of a combination of possible caldera resurgence and ongoing arc-related uplift in the region.

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