| DOI: | 10.1306/07311212071
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| Scopus记录号: | 2-s2.0-84876122013
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| 论文题名: | Sedimentologic and diagenetic controls on pore-network characteristics of Oligocene-Miocene ramp carbonates (Majella Mountain, central Italy) |
| 作者: | Rustichelli A.; Tondi E.; Agosta F.; Di Celma C.; Giorgioni M.
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| 刊名: | AAPG Bulletin
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| ISSN: | 0149-1711
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| EISSN: | 1558-9441
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| 出版年: | 2013
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| 发表日期: | 2013
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| 卷: | 97, 期:3 | | 起始页码: | 487
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| 结束页码: | 524
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| 语种: | 英语
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| Scopus关键词: | Deposits
; Grain size and shape
; Benthic foraminifera
; Central Italy
; Macro-porosity
; Majella Mountain
; Oligocene-Miocene carbonates
; Planktonic foraminifera
; Porosity reduction
; Prediction of reservoir
; Carbonates
; carbonate
; cementation
; diagenesis
; facies
; grainstone
; laboratory method
; macropore
; planktonic foraminifera
; porosity
; sedimentology
; Abruzzi
; Apennines
; Italy
; Majella Mountains
; Bryozoa
; Echinoida
; Foraminifera
; Lepidocyclina
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| Scopus学科分类: | Energy
; Earth and Planetary Sciences
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| 英文摘要: | This article addresses the controls exerted by sedimentologic and diagenetic factors on the preservation and modification of pore-network characteristics (porosity, pore types, sizes, shapes, and distribution) of carbonates belonging to the Bolognano Formation. This formation, exposed at the Majella Mountain, Italy, is composed of Oligocene-Miocene carbonates deposited in middle- to outer-ramp settings. The carbonates consist of (1) grainstones predominantly composed of either larger benthic foraminifera, especially Lepidocyclina, or bryozoans; (2) grainstones to packstones with abundant echinoid plates and spines; and (3) marly wackestones to mudstones with planktonic foraminifera. The results of this field- and laboratory-based study are consistent with skeletal grain assemblages, grain sizes, sorting, and shapes, all representing the sedimentologic factors responsible for high values of connected primary macroporosity in grainstones deposited on the high-energy, middle to proximal outer ramp. Cementation, responsible for porosity reduction and overall macropore shape and distribution in grainstones to packstones deposited on the intermediate outer ramp, was mainly dependent on the following factors: (1) amount of echinoid plates and spines, (2) grain size, (3) grain sorting and shapes, and (4) clay amount. Differently, in the wackestones to mudstones, laid down on the low-energy, distal outer ramp, matrix is the key sedimentologic factor responsible for low values of scattered macroporosity and dominance of microporosity. The aforementioned results may be useful to improve the prediction of reservoir quality by means of mapping, simulating, and assessing individual carbonate facies with peculiar pore-network characteristics. ©2013. The American Association of Petroleum Geologists. All rights reserved. |
| URL: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-84876122013&doi=10.1306%2f07311212071&partnerID=40&md5=47a0edf6f2f765331ff8c17e9f1b85f9
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| Citation statistics: |
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| 资源类型: | 期刊论文
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| 标识符: | http://119.78.100.158/handle/2HF3EXSE/13281
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| Appears in Collections: | 过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响
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| Recommended Citation: | |
Rustichelli A.,Tondi E.,Agosta F.,et al. Sedimentologic and diagenetic controls on pore-network characteristics of Oligocene-Miocene ramp carbonates (Majella Mountain, central Italy)[J]. AAPG Bulletin,2013-01-01,97(3)
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