Mecabrecial

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Nubrigyn algal reefs (Devonian), eastern Australia: Allochthonous blocks and megabreccias P. J. C O N A G H A N School of Earth Sciences, Macquarie E. W . M O U N T J O Y Department of Geological Sciences, J^ A^ TALENT^^ D. E. O W E N

J Department

School

of Earth Sciences,

of Geology,

Bowling

University, North McGill University,

Macquarie

University,

Ryde, New South Wales, 2113, Montreal, Quebec H3C 3GI,

North

Green State University,

Bowling

ABSTRACT The widely known Lower Devonian "algal reef' limestones of the Nubrigyn Formation, New South Wales, are enormous allochthonous blocks contained within a 400-m interval of interbedded mudstones, allodapic carbonates, and megabreccias that form part of a 5,000-m succession of Lower Devonian volcanics and flysch. Previous workers have interpreted these massive limestone bodies to be algal bioherms that developed in sublittoral to littoral environments around volcanic pedestals on a "Nubrigyn shelf." The allochthonous nature of the limestone bodies is clearly indicated by (1) occurrence of a wide range of clast sizes, as much as 1 km across; (2) presence of a wide range of clast types and sizes in close juxtaposition; (3) discordance between stratigraphic facing of the large limestone bodies and stratification in surrounding beds; (4) lack of distinctive and regular facies changes within the limestone bodies, particularly near their margins; (5) abrupt and random truncation of internal fabrics at block margins; (6) lack of an autochthonous volcanic foundation for the "reefs"; and (7) anomalous lithofacies association of the massive bodies of shoalwater limestone with enclosing flysch. The limestones initially formed in a shoal-water carbonate complex to the west upon a geologically persistent volcanic archipelago, the Molong Arch, where source rocks for the Nubrigyn megaclasts and megabreccias crop out in the Lower Devonian Garra Formation and Cuga Burga Volcanics. The Nubrigyn megaclasts were transported eastward as debris flows into the adjacent and relatively deep water Hill End Trough after dislodgement from the eastern margin of the Garra shelf. Megaclasts isolated within hemipelagic mudstones and flysch were presumably transported by sliding or rolling. The loci of accumulation of the debris flows and exotic blocks occupy a meridional basin-margin position between the Molong Arch to the west and the predominantly turbidite-filled Hill End Trough to the east. Other debris-flow megabreccias, many previously unrecognized as having been transported and deposited in this manner, occur in the Paleozoic rocks of the Tasman mobile belt of eastern Australia. Key words: sedimentology, stratigraphy, algal limestone, submarine debris flow, limestone megabreccia, megaclast, turbidite, allodapic limestone, Tasman mobile belt, Australia, Devonian, Nubrigyn. INTRODUCTION K. H. Wolf (1965a, 1965b, 1965c, 1965d; Chilingar and others, 1967) has brought to prominence some Australian Lower Devonian limestones that he interpreted as algal reefs because of their distinctive textures. Wolf recognized algal components in three contemporary Lower Devonian units in the area between the towns of Orange and Wellington in east-central New South Wales (Fig.

Ryde,

New South

Green,

Ohio

Australia Canada

Wales, 2113,

Australia

43403

1): the Red Hill Formation, the Nubrigyn Formation, and the Tolga Calcarenite. He envisaged the first two of these units as consisting of shoal-water reef complexes and the third as an associated flanking accumulation of basin-margin carbonate turbidite. The Nubrigyn Formation is the most extensive and best exposed of the three units (Figs. 1, 2). Because of the international prominence of the Nubrigyn Formation in the carbonate literature and because of our interest in reef problems, the "algal reefs" and associated sediments of this formation were re-examined. Our studies indicate that the "algal reefs" are allochthonous (Mountjoy and others, 1972a). Thus, although important in themselves, the earlier petrographic and paleoenvironmental studies of the "algal-reef' limestones (Wolf, 1965a, 1965b, 1965c; Johnson, 1964) apply to former bank-margin situations, not to an autochthonous complex of algal patch reefs, as was widely reported or inferred (Packham, 1958, 1968a, 1969; Wolf, 1963, 1965a; Johnson, 1964; Strusz, 1967; Brown and others, 1968; Hatch and Rastall, 1971; Pogson, 1972). The carbonate terminology used throughout this paper is largely that of Dunham (1962) and Folk (1959). The terminology used in reference to breccias, megabreccias, allodapic carbonates, carbonate buildups, and the like follows that employed by Jones (1970), Cook and others (1972), and Mountjoy and others (1972b). The definitions given in Appendix 1 clarify the meanings used here. This paper is based on field work on the Nubrigyn Formation in July 1970 by Talent and in the first half of 1971 by Mountjoy, Talent, Conaghan, Owen, and Edgecombe and on work during and since 1972 by Edgecombe and Conaghan. Some additional data were kindly supplied by J. G. Byrnes (1972, unpub. maps; see also Morton, 1974). The best outcrops of the formation occur in the vicinity of Canobla (the type region; Fig. 3), and much critical data come from this area. REGIONAL SETTING The Lower Devonian formations of the Orange-Wellington area of New South Wales occur within the Paleozoic Tasman mobile belt — a region of eastern Australia characterized by a history of precratonic development prior to Late Devonian time. These units crop out along the flanks of the meridional Molong Arch, a remarkably persistent north-south structure with a well-documented history of recurrent volcanism and carbonate buildup throughout Ordovician to Early Devonian time (Figs. 1, 2). The paleogeography of the Tasman mobile belt in Silurian and Early Devonian times comprised several such arches or volcanic archipelagoes separated by intervening sedimentary troughs. Contrasts in lithofacies, aggregate thickness, and degree of tectonic disturbance characterize sedimentary deposits regarded as having formed respectively within the troughs and on the highs and serve to define the areal extent of the major paleotopographic elements (Fig. 1, A).

Geological Society of America Bulletin, v. 87, p. 5 1 5 - 5 3 0 , 14 figs., April 1976, Doc. no. 60404.

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