DOI: 10.1016/j.gloplacha.2012.05.026
论文题名: Aggradation and progradation controlled clinothems and deep-water sand delivery model in the Neogene lake pannon, Makó Trough, Pannonian Basin, SE Hungary
作者: Sztanó O. ; Szafián P. ; Magyar I. ; Horányi A. ; Bada G. ; Hughes D.W. ; Hoyer D.L. ; Wallis R.J.
刊名: Global and Planetary Change
ISSN: 0921-8341
出版年: 2013
卷: 103, 期: 1 起始页码: 149
结束页码: 167
语种: 英语
英文关键词: Lacustrine
; Messinian
; Sediment supply
; Shelf-margin trajectory
; Turbidite systems
Scopus关键词: Highstand systems tract
; Lacustrine
; Messinian
; Sand accumulation
; Sediment supply
; Seismic resolution
; Turbidite systems
; Turbidity current
; lacustrine
; Coastal zones
; Deposits
; Drops
; Floors
; Lithology
; Ocean currents
; Petroleum geology
; Sand
; Sediment transport
; Sedimentology
; Seismology
; Stratigraphy
; Trajectories
; Well logging
; Lakes
; amplitude
; deep water
; geoaccumulation
; geomorphology
; lacustrine deposit
; lithology
; Messinian
; Neogene
; seismic data
; three-dimensional modeling
; turbidity current
; volume
; aggradation
; Miocene
; morphology
; Pliocene
; progradation
; shelf break
; turbidite
; Pannonian Basin
; Zanclea
英文摘要: In the Late Miocene-Early Pliocene Lake Pannon, regression went on for about 6 Ma. Sediments arriving from the Alpine-Carpathian source area were partly accumulated on the flat-lying morphological shelf of the lake, whereas other portions of the sediment were passing through to the slope and deposited on the deep basin floor. The height of the slope exceeded 400-500mbased on correlatedwell and seismic data. An extended 3D seismic volume covering the Makó Trough, one of the largest and deepest depressionswithin the Pannonian Basin, provided an opportunity to study sequences and shelf-margin trajectories generated as a result of continuous slope advancement. The lithology of these shelf, slope and basin centre deposits was inferred fromseven well logs and 220 mcorematerial. In the Makó Trough the southeastward migrating shelf-margin was formed by alternating aggradational and progradational clinothems. Aggradational clinothems, i.e. aggradation accompanied by subordinate progradation, are characterised by rising shelf-margin trajectories. The shelf built up from inner-shelf to shelf-edge deltaic lobes which compose a few dozen metre thick coarsening-up units. The majority of the sand, however, was transported by effective turbidity currents through leveed channels into the basin, and deposited as thick, extended slopedetached turbidite lobes up to a distance of 30 km from the shelf edge. In aggradational clinothems both the shelf and the basin floor accreted vertically. Development of progradational clinothems resulted in horizontal (flat) shelf-margin trajectories. Corresponding reflections toplap at the shelf edge and downlap within a distance of few kilometres from the toe of the slope. The shelf was bypassed, sediments accumulated on the slope and directly at the slope-toe region as small simple lobes. Short-distance transportwas the result of clay-poor, non-effective turbidity currents. Consequently, the thickness of coeval basin-centre sediments remained negligible in progradational clinothems. Alternations of rising and horizontal shelf margin trajectories indicate that the climate- and subsidence-controlled lacustrine base-level rose continuously, though at varying rates. Descending trajectories were not observed. It means that base-level drops larger in amplitude than the seismic resolution (20-30 m), did not occur during the studied time interval, i.e. at 7-5 Ma ago, approximately corresponding to the Messinian age. As a result, major forced-regressive wedges or lowstand fans did not develop. This is in contrast with former stratigraphic models claiming that several 3rd-order sequences, including the intra-Messinian unconformity supposedly induced by hundred metres large lake-level drop, developed in Lake Pannon with significant volume of lowstand deposits as turbidites. Instead, aggradational and progradational clinothems are interpreted as fourth-order transgressive, early and late highstand systems tracts. These incomplete sequences represent less than 100 kyr time intervals. Due to climate control both on high rate of sediment supply and thewater budget of Lake Pannon, conditions were more favourable for deposition of large volumes of well-developed turbidite systems during base-level rise than during stagnation or minor base-level fall. Therefore, sand delivery to the basin centre was at maximum during the early highstand aggradational stage and atminimum during the late highstand progradational stage. The timing and position of sand accumulation in the Makó Trough of Lake Pannon is different from those predicted by "traditional" sequence stratigraphic considerations. © 2012 Elsevier B.V. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84878215257&doi=10.1016%2fj.gloplacha.2012.05.026&partnerID=40&md5=2600ab39526acd1ad877a5a2345e8ef5
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11247
Appears in Collections: 全球变化的国际研究计划
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作者单位: Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány Péter sétany 1/c, 1117 Budapest, Hungary
Recommended Citation:
Sztanó O.,Szafián P.,Magyar I.,et al. Aggradation and progradation controlled clinothems and deep-water sand delivery model in the Neogene lake pannon, Makó Trough, Pannonian Basin, SE Hungary[J]. Global and Planetary Change,2013-01-01,103(1).