洛阳龙门地区中寒武统张夏组下部遗迹组构及其沉积环境

齐永安; 王敏; 李妲; 孙长彦; 代明月

doi:10.3799/dqkx.2012.078

Volume 37 Issue 4

Jul. 2012

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Article Navigation > Earth Science > 2012 > 37(4): 693-706

QI Yong-an, WANG Min, LI Da, SUN Chang-yan, DAI Ming-yue, 2012. Ichnofabrics and Their Sedimentary Environments from the Lower Part of the Middle Cambrian Zhangxia Formation, Longmen Area, Luoyang City. Earth Science, 37(4): 693-706. doi: 10.3799/dqkx.2012.078

Citation:

QI Yong-an, WANG Min, LI Da, SUN Chang-yan, DAI Ming-yue, 2012. Ichnofabrics and Their Sedimentary Environments from the Lower Part of the Middle Cambrian Zhangxia Formation, Longmen Area, Luoyang City. Earth Science, 37(4): 693-706. doi: 10.3799/dqkx.2012.078

Citation:

QI Yong-an, WANG Min, LI Da, SUN Chang-yan, DAI Ming-yue, 2012. Ichnofabrics and Their Sedimentary Environments from the Lower Part of the Middle Cambrian Zhangxia Formation, Longmen Area, Luoyang City. Earth Science, 37(4): 693-706. doi: 10.3799/dqkx.2012.078

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Ichnofabrics and Their Sedimentary Environments from the Lower Part of the Middle Cambrian Zhangxia Formation, Longmen Area, Luoyang City

doi: 10.3799/dqkx.2012.078

Key Laboratory of Biogenic Traces and Sedimentary Minerals of Henan Province, Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo 454000, China

Received Date: 2011-12-13
Available Online: 2021-10-13
Publish Date: 2012-07-15

Abstract

Abstract

The Zhangxia Formation in the Longmen area, Luoyang City, was a set of deposited thin-bedded microcrystalline limestone and thick-bedded oolitic limestone, with abundant bioturbation. Based on sedimentology and ichnology characteristics, six ichnofabrics were determined, namely from the bottom up, Planolites montanus ichnofabric in low energy, subtidal carbonate platform; Palaeophycus tubularis-Thalassinoides horizontalis ichnofabric in shallow, medium energy, subtidal carbonate platform; Skolithos linearis-Planolites montanus ichnofabric in onshore oolitic shoals, inter flat and fore shoals of oolitic platform with alternation of high and low energy; blurry bioturbation ichnofabric in deeper water, lower energy of open platform; Macaronichnus segregatis ichnofabric in oolitic shoals with high energy and Palaeophycus heberti ichnofabric in subtidal restricted platform with low energy. Zhangxia Formation in Longmen area developed from carbonate platform without oolitic shoals to with oolitic shoals. The sedimentary environment evolved from onshore oolitic shoals to open platform without oolitic shoals, and finally ended up with platform oolitic shoals and restricted platform with the regression.
- ichnofabric,
- bioturbation,
- carbonate rock,
- Middle Cambrian,
- Zhangxia Formation,
- sedimentology,
- stratigraphy

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References(44)

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Ichnofabrics and Their Sedimentary Environments from the Lower Part of the Middle Cambrian Zhangxia Formation, Longmen Area, Luoyang City

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