東華大學圖書館 |

Language: English

Help

回圖書館首頁

手機版館藏查詢

Back

Switch To: Labeled | MARC Mode | ISBD

Linked to FindBook

Google Book

Amazon

博客來

Tidal Influence in a Prograding Cretaceous Coastal Plain : = Hell Creek Formation near Marmarth, North Dakota.

Record Type:	Electronic resources : Monograph/item
Title/Author:	Tidal Influence in a Prograding Cretaceous Coastal Plain :/
Reminder of title:	Hell Creek Formation near Marmarth, North Dakota.
Author:	Khatri, Samantha.
Description:	1 online resource (198 pages)
Notes:	Source: Masters Abstracts International, Volume: 83-12.
Contained By:	Masters Abstracts International83-12.
Subject:	Sedimentary geology. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=28968008click for full text (PQDT)
ISBN:	9798834004189

Tidal Influence in a Prograding Cretaceous Coastal Plain : = Hell Creek Formation near Marmarth, North Dakota.
Khatri, Samantha.

Tidal Influence in a Prograding Cretaceous Coastal Plain :Hell Creek Formation near Marmarth, North Dakota. - 1 online resource (198 pages)

Source: Masters Abstracts International, Volume: 83-12.

Thesis (M.S.)--University of Georgia, 2022.

Includes bibliographical references

The Hell Creek Formation in western north America is understood to represent an aggrading fluvial system that deposited during the end of the Western Interior Seaway. The facies of the Hell Creek Formation near Marmarth, North Dakota were measured and described at eleven outcrops to develop a sequence stratigraphic framework. Based on the relationship of channel deposits and paleosols, the Hell Creek Formation is divided into three zones that are related to the lateral movement of the ancient shoreline. Tidally generated structures are present and indicate that several facies of the Hell Creek Formation were influenced by tides. This is significant because tidal influence has not been previously interpreted in the Hell Creek Formation. The recognition of tidal influence provides insight into the Hell Creek landscape, and in combination with the three identified zones, indicates that the movement of the ancient shoreline and the Hell creek system was prograding and aggrading.

Electronic reproduction.
Ann Arbor, Mich. :
ProQuest,
2023

Mode of access: World Wide Web

ISBN: 9798834004189Subjects--Topical Terms:

3173828
Sedimentary geology.
Subjects--Index Terms:

AvulsionIndex Terms--Genre/Form:

542853
Electronic books.

Tidal Influence in a Prograding Cretaceous Coastal Plain : = Hell Creek Formation near Marmarth, North Dakota.
LDR:02378nmm a2200397K 4500 001 2358477
005 20230814100725.5
006 m o d
007 cr mn ---uuuuu
008 241011s2022 xx obm 000 0 eng d
020 $a 9798834004189
035 $a (MiAaPQ)AAI28968008
035 $a AAI28968008
040 $a MiAaPQ $b eng $c MiAaPQ $d NTU
100 1 $a Khatri, Samantha. $3 3699005
245 1 0 $a Tidal Influence in a Prograding Cretaceous Coastal Plain : $b Hell Creek Formation near Marmarth, North Dakota.
264 0 $c 2022
300 $a 1 online resource (198 pages)
336 $a text $b txt $2 rdacontent
337 $a computer $b c $2 rdamedia
338 $a online resource $b cr $2 rdacarrier
500 $a Source: Masters Abstracts International, Volume: 83-12.
500 $a Advisor: Holland, Steven M.
502 $a Thesis (M.S.)--University of Georgia, 2022.
504 $a Includes bibliographical references
520 $a The Hell Creek Formation in western north America is understood to represent an aggrading fluvial system that deposited during the end of the Western Interior Seaway. The facies of the Hell Creek Formation near Marmarth, North Dakota were measured and described at eleven outcrops to develop a sequence stratigraphic framework. Based on the relationship of channel deposits and paleosols, the Hell Creek Formation is divided into three zones that are related to the lateral movement of the ancient shoreline. Tidally generated structures are present and indicate that several facies of the Hell Creek Formation were influenced by tides. This is significant because tidal influence has not been previously interpreted in the Hell Creek Formation. The recognition of tidal influence provides insight into the Hell Creek landscape, and in combination with the three identified zones, indicates that the movement of the ancient shoreline and the Hell creek system was prograding and aggrading.
533 $a Electronic reproduction. $b Ann Arbor, Mich. : $c ProQuest, $d 2023
538 $a Mode of access: World Wide Web
650 4 $a Sedimentary geology. $3 3173828
650 4 $a Geology. $3 516570
653 $a Avulsion
653 $a Cretaceous
653 $a Marine transition zone
653 $a Hell Creek Formation
653 $a Nonmarine
653 $a Sequence stratigraphy
655 7 $a Electronic books. $2 lcsh $3 542853
690 $a 0594
690 $a 0372
710 2 $a ProQuest Information and Learning Co. $3 783688
710 2 $a University of Georgia. $b Geology - MS. $3 3699006
773 0 $t Masters Abstracts International $g 83-12.
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=28968008 $z click for full text (PQDT)