干旱区生态环境知识资源中心(Arid): Cyclic carbonate-siliciclastic sedimentation in a shallow marine to coastal environment (latest Kimmeridgian-early Tithonian, Galve sub-basin, Spain)

Arid

DOI	10.1007/s41513-018-00098-1
	Cyclic carbonate-siliciclastic sedimentation in a shallow marine to coastal environment (latest Kimmeridgian-early Tithonian, Galve sub-basin, Spain)
	Val, Jorge 1; Aurell, Marcos 1; Badenas, Beatriz 1; Castanera, Diego 1; Subias, Saul 2
通讯作者	Val, Jorge
来源期刊	JOURNAL OF IBERIAN GEOLOGY
ISSN	1698-6180
EISSN	1886-7995
出版年	2019
卷号	45 期号:1 页码:195-222
英文摘要	The sedimentological analysis of the uppermost Kimmeridgian to lower Tithonian Villar del Arzobispo Formation (Galve sub-basin, NE Spain) has allowed characterizing different carbonate, mixed and siliciclastic facies deposited in coastal to shallow marine areas. Its age calibration has been specified on the basis of new biostratigraphic and chemostratigraphic data. Four successive sequences (30-80 m thick) characterized by the relative dominance of carbonate and siliciclastic facies reflect a sedimentary change from reciprocal to mixed carbonate-siliciclastic sedimentation. Sequences 1 and 2 are reciprocal sedimentation cycles from carbonate-dominated (muddy coastal plain-carbonate lagoon) to siliciclastic coasts (muddy coastal plain-wave dominated delta). Sequence S3 is also reciprocal, from a mixed carbonate-siliciclastic coastal plain-lagoon at the lower part to a wave-dominated delta on top. A mixed carbonate-siliciclastic coastal plain-lagoon characterizes the entire sequence 4. Climate and tectonics controlled carbonate deposition and siliciclastic supply. Reciprocal sedimentation in sequences 1-3 was controlled by orbitally-driven climate changes (from arid to humid conditions) on the age range of long-term eccentricity cycles. A greater imprint of extensional synsedimentary tectonics at the upper part of sequence 3 and during sequence 4 is thought to be the main factor producing the gradual opening of the sub-basin to the wave influence and a more continuous siliciclastic supply, then controlling the change from reciprocal to mixed sedimentation and obliterating the possible imprint of orbitally-induced climatic changes.
英文关键词	Carbonate-siliciclastic Coastal transition Sequences Synsedimentary tectonics Upper Jurassic Galve sub-basin
类型	Article
语种	英语
国家	Spain
收录类别	SCI-E
WOS记录号	WOS:000459558800012
WOS关键词	SEQUENCE STRATIGRAPHY ; BASIN ; EVOLUTION ; FACIES ; TERUEL ; CHRONOSTRATIGRAPHY ; TRANSITION ; PATTERNS ; CLIMATE ; OOIDS
WOS类目	Geology
WOS研究方向	Geology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/217194
作者单位	1.Univ Zaragoza, IUCA, Dept Ciencias Tierra, Zaragoza 50009, Spain; 2.Repsol Explorac, Campus Repsol, Madrid 28045, Spain
推荐引用方式 GB/T 7714	Val, Jorge,Aurell, Marcos,Badenas, Beatriz,et al. Cyclic carbonate-siliciclastic sedimentation in a shallow marine to coastal environment (latest Kimmeridgian-early Tithonian, Galve sub-basin, Spain)[J],2019,45(1):195-222.
APA	Val, Jorge,Aurell, Marcos,Badenas, Beatriz,Castanera, Diego,&Subias, Saul.(2019).Cyclic carbonate-siliciclastic sedimentation in a shallow marine to coastal environment (latest Kimmeridgian-early Tithonian, Galve sub-basin, Spain).JOURNAL OF IBERIAN GEOLOGY,45(1),195-222.
MLA	Val, Jorge,et al."Cyclic carbonate-siliciclastic sedimentation in a shallow marine to coastal environment (latest Kimmeridgian-early Tithonian, Galve sub-basin, Spain)".JOURNAL OF IBERIAN GEOLOGY 45.1(2019):195-222.