| DOI: | 10.1306/06191312170
|
| Scopus记录号: | 2-s2.0-84888625301
|
| 论文题名: | Topographic and sea level controls on oolite-microbialite-coralgal reef sequences: The terminal carbonate complex of southeast Spain |
| 作者: | Goldstein R.H.; Franseen E.K.; Lipinski C.J.
|
| 刊名: | AAPG Bulletin
|
| ISSN: | 0149-1631
|
| EISSN: | 1558-9361
|
| 出版年: | 2013
|
| 发表日期: | 2013
|
| 卷: | 97, 期:11 | | 起始页码: | 1997
|
| 结束页码: | 2034
|
| 语种: | 英语
|
| Scopus关键词: | Carbonate complexes
; Intermediate substrates
; Marine organisms
; Oolite reservoir
; Relative sea level
; Relative sea level rise
; Sealevel change
; Substrate positions
; Carbonation
; Marine biology
; Reefs
; Stratigraphy
; Substrates
; Sea level
; carbonate
; coast
; facies
; glacioeustacy
; grainstone
; highstand
; lithofacies
; Messinian
; Miocene
; ooid
; paleotopography
; reef
; sea level
; sea level change
; substrate
; thrombolite
; Spain
|
| Scopus学科分类: | Energy
; Earth and Planetary Sciences
|
| 英文摘要: | The terminal carbonate complex of southeast Spain is a Miocene (Messinian) unit of oolite, microbialite, and coralgal reels deposited in association with glacioeustasy and evaporitic drawdown. The relationship between paleotopography and sea level history is useful for prediction of microbialite and oolite reservoir facies in the subsurface. Four sequences record sea level change with minimum amplitudes of 32-77 m (105-253 ft). Sequences commonly have local basal stromatolites overlain by local thrombolites, ooid grainstone, volcaniclastic-rich planar-bedded ooid grainstone, and fenestral ooid grainstone. At low substrate positions, thrombolite boundstones are thicker and laterally more continuous than at higher positions. At intermediate substrate positions (relative to sea level history), sequences have a build-and-fill architecture, characterized by a reliefbuilding phase and a relief-filling phase, with thin sequences draping paleotopography. Microbialites dominate during the relative sea level rises and build topographic relief. Oolites dominate during the relative sea level falls and fill topographic relief. At higher substrate positions, close to highstand, sequences thicken and yield stratigraphic character that is inconsistent with a build-and-fill model. Apparently, the build-and-fill model requires an intermediateelevation substrate position and nonoptimal carbonate productivity during rapid sea level change. Sequences progressively show increasing diversity and more normal marine organisms, possibly caused by decreasing aridity. Lithofacies of the La Molata area show evidence of more restricted conditions compared to the La Rellana-Ricardillo area lithofacies, likely because La Molata was in an embayment. These results show that distribution of oolite, microbialite, and reef facies are predictable given known interaction among sea level, paleotopography of the depositional surface (substrate), and coastline configuration. © 2013. The American Association of Petroleum Geologists. All rights reserved. |
| URL: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-84888625301&doi=10.1306%2f06191312170&partnerID=40&md5=a07e2c87d7a8a8c7a4ea6a83dcd30677
|
| Citation statistics: |
|
| 资源类型: | 期刊论文
|
| 标识符: | http://119.78.100.158/handle/2HF3EXSE/13201
|
| 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
|
|
There are no files associated with this item.
|
| Recommended Citation: | |
Goldstein R.H.,Franseen E.K.,Lipinski C.J.. Topographic and sea level controls on oolite-microbialite-coralgal reef sequences: The terminal carbonate complex of southeast Spain[J]. AAPG Bulletin,2013-01-01,97(11)
|
|
|