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      Data report: moisture and density analysis and ultrasonic velocity, Hole U1513E, IODP Expedition 369

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      Proceedings of the International Ocean Discovery Program
      International Ocean Discovery Program

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          Abstract

          In this data report, we present postcruise petrophysical measurement results for Hole U1513E. During International Ocean Discovery Program (IODP) Expedition 369, five holes were drilled at Site U1513 on the Naturaliste Plateau offshore southwest Australia. The last and deepest hole, U1513E, recovered a volcanic sequence (Lithostratigraphic Unit VI) consisting of basalt flows, dolerite dikes, and volcaniclastic beds. Because of time constraints, moisture and density (MAD) measurements were not possible on board for Hole U1513E. To obtain bulk (wet), dry, and grain density and porosity data, we performed the MAD analysis on 25 core samples collected from Hole U1513E after the expedition. Among these samples, five were selected to measure ultrasonic velocity and dynamic Poisson’s ratio. Six additional samples from Hole U1513D were analyzed to compare with shipboard data to validate the postcruise measurements. The results are compatible with shipboard data in individual lithologic units. Samples of relatively fresh rocks show bulk and dry density values near 2.5 g/cm3 and porosity near 10%, whereas altered basalts and volcaniclastics exhibit lower values of bulk and dry density and higher values of porosity. Grain density varies between 2.6 and 3.3 g/cm3. S-wave velocity ranges from 934 to 3135 m/s, which accompanies variable dynamic Poisson’s ratio between 0.1 and 0.35.

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          Early Cretaceous subsidence of the Naturaliste Plateau defined by a new record of volcaniclastic-rich sequence at IODP Site U1513

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            Expedition 369 methods

            This chapter documents the procedures and methods used in the shipboard laboratories during International Ocean Discovery Program (IODP) Expedition 369. This introductory section in particular provides a rationale for the site locations and an overview of IODP depth conventions, curatorial procedures, and general core handling/analyses during Expedition 369. Subsequent sections describe specific laboratory procedures and instruments in more detail. This information only applies to shipboard work described in the Proceedings volume; methods used in shore-based analyses of Expedition 369 samples and/or data will be described in various scientific contributions in the open peer-reviewed literature and the Expedition Research Results chapters of this Proceedingsvolume.
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              Site U1513

              International Ocean Discovery Program (IODP) Site U1513 (33°47.6084′S, 112°29.1338′E) lies at ~2800 m water depth on the western margin of the Mentelle Basin. This Cretaceous basin is probably underlain by synrift Permian to Jurassic sediment that is part of an early rifting event that extends along the western margin of Australia. Following the separation of India from Australia/Antarctica in the Early Cretaceous, the basin underwent a period of rapid thermal subsidence with deposition of deltaic sediment, shale, and claystone sequences, followed by deep-water chalks and limestones. The current seabed is composed of Paleogene/Neogene/Quaternary oozes that sit unconformably on the Cretaceous. Objectives for coring Site U1513 were to obtain a continuous Late Cretaceous sediment record in the Mentelle Basin (adjacent to the Naturaliste Plateau) to better document the rise and fall of the Cretaceous hot greenhouse climate at southern high paleolatitudes (~60°S), characterize how oceanographic conditions changed during the Cenozoic opening of the Tasman Gateway and the restriction of the Indonesian Gateway, and recover breakup-related volcanic rocks from the base of the sedimentary succession to provide age control on the onset and duration of volcanism in the Mentelle Basin. An important goal was to obtain a complete Oceanic Anoxic Event (OAE) 2 sequence across the Cenomanian/Turonian boundary to characterize associated biotic, oceanographic, and climatic changes. The Site U1513 sequence will be compared with coeval Expedition 369 sections cored elsewhere in the Mentelle Basin and at Site U1512 from the Great Australian Bight. The sequence will also be compared with other IODP and industry data from the Western Australia margin and the Great Australian Bight to identify any regional differences in the geochemical and biological responses to the OAEs and Cretaceous and Neogene ocean circulation history. Site U1513 is located 1.1 km east-northeast of Deep Sea Drilling Project (DSDP) Leg 26 Site 258, which was spot-cored (20% recovery) in the Cretaceous section (Luyendyk and Davies, 1975). Site 258 failed to recover samples from the OAE 2 interval and stopped short of penetrating the basalts; however, it did provide valuable information about the lithologies and depths of expected key horizons. The goals at Site U1513 were to complete the gaps of Site 258, to recover a complete sequence of OAE 2, and to recover unaltered samples of the Naturaliste Plateau basalts. Coring in five holes achieved high recovery (80.8%), including a likely sequence from the OAE 2 interval, a nearly complete section of upper Neogene deposits, and samples of altered and possibly unaltered basaltic rocks. Recovered samples will provide new insights on the paleoceanographic evolution during the Cretaceous greenhouse at southern high paleolatitudes, on the timing of breakup of India from Australia/Antarctica, and on the processes of rifting formation and basin subsidence in magma-poor margins.
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                Author and article information

                Journal
                10.14379/iodp.proc.369.2019
                Proceedings of the International Ocean Discovery Program
                International Ocean Discovery Program
                2377-3189
                12 April 2021
                Article
                10.14379/iodp.proc.369.204.2021
                a7918a40-fc59-43ca-a910-1b7d75ffb498

                This work is licensed under a Creative Commons Attribution 4.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

                History

                Earth & Environmental sciences,Oceanography & Hydrology,Geophysics,Chemistry,Geosciences

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