001438826 000__ 03828cam\a2200589\i\4500 001438826 001__ 1438826 001438826 003__ OCoLC 001438826 005__ 20230309004356.0 001438826 006__ m\\\\\o\\d\\\\\\\\ 001438826 007__ cr\un\nnnunnun 001438826 008__ 210812s2021\\\\sz\a\\\\ob\\\\000\0\eng\d 001438826 019__ $$a1263873757 001438826 020__ $$a9783030793975$$q(electronic bk.) 001438826 020__ $$a3030793974$$q(electronic bk.) 001438826 020__ $$z9783030793968 001438826 020__ $$z3030793966 001438826 0247_ $$a10.1007/978-3-030-79397-5$$2doi 001438826 035__ $$aSP(OCoLC)1263662888 001438826 040__ $$aYDX$$beng$$erda$$epn$$cYDX$$dGW5XE$$dOCLCO$$dEBLCP$$dOCLCF$$dOCLCO$$dOCLCQ$$dCOM$$dOCLCQ 001438826 043__ $$an-mx--- 001438826 049__ $$aISEA 001438826 050_4 $$aQE615.5.M6$$bL38 2021 001438826 08204 $$a557.2/13$$223 001438826 1001_ $$aLawton, Timothy Frost,$$eauthor. 001438826 24513 $$aLa Popa Basin, Nuevo León and Coahuila, Mexico :$$bhalokinetic sequences and diapiric structural kinematics in the field /$$cTimothy Lawton, Katherine Giles, Mark Rowan. 001438826 264_1 $$aCham :$$bSpringer,$$c[2021] 001438826 264_4 $$c©2021 001438826 300__ $$a1 online resource :$$billustrations (chiefly color) 001438826 336__ $$atext$$btxt$$2rdacontent 001438826 337__ $$acomputer$$bc$$2rdamedia 001438826 338__ $$aonline resource$$bcr$$2rdacarrier 001438826 4901_ $$aSpringer geology. Springer geology field guides,$$x2730-7344 001438826 504__ $$aIncludes bibliographical references. 001438826 5050_ $$aPart 1: General Information -- Chapter 1. Opening Statement -- Chapter 2. General Access and Logistics -- Chapter 3. Safety Instructions -- Chapter 4. Emergency Contacts -- Part 2: Introduction -- Chapter 5. Regional Tectonic Setting -- Chapter 6. Tectonic Provinces -- Chapter 7. Timing of Deformation in the Mexican Foreland -- Chapter 8 -- La Popa Basin Stratigraphy -- Chapter 9. Halokinetic Sequences and Composite -- Chapter 10- Halokinetic Sequences -- Chapter 11- Application to Deepwater Salt Provinces. 001438826 506__ $$aAccess limited to authorized users. 001438826 520__ $$aThis book describes the two excursions accessed from the Monterrey International Airport on the north side of Monterrey, Nuevo León, Mexico. Excellent exposures of salt diapirs and flanking strata in La Popa basin, northeastern Mexico, contain world-class examples of salt-sediment interaction that provided the basis for the concept of halokinetic sequences. The basin also contains one of the first secondary salt welds described in outcrop. Two one-day excursions described here provide an easily accessible overview of salt-sediment relations within a short distance of Monterrey, Nuevo León, Mexico. Excursion 1 constitutes an introduction to basin stratigraphy, an introduction to halokinetic sequences at El Papalote diapir, and a visit to a salt-cored detachment fold near Hidalgo, Nuevo León. Excursion 2 is a visit to La Popa salt weld, where stops at several parts of the weld permit comparison of different structural styles developed along the weld. Each excursion begins and ends at the Marriott Courtyard Aeropuerto Hotel, near the Monterrey airport. 001438826 588__ $$aOnline resource; title from PDF title page (SpringerLink, viewed August 20, 2021). 001438826 650_0 $$aSalt tectonics$$zMexico$$zMonterrey. 001438826 650_0 $$aBasins (Geology)$$zMexico$$zMonterrey. 001438826 650_6 $$aTectonique du sel$$zMexique$$zMonterrey. 001438826 650_6 $$aBassins (Géologie)$$zMexique$$zMonterrey. 001438826 655_0 $$aElectronic books. 001438826 7001_ $$aGiles, Katherine A.,$$eauthor. 001438826 7001_ $$aRowan, M. G.$$q(Mark Geoffrey),$$eauthor. 001438826 77608 $$iPrint version: $$z3030793966$$z9783030793968$$w(OCoLC)1252961245 001438826 830_0 $$aSpringer geology.$$pSpringer geology field guides.$$x2730-7344 001438826 852__ $$bebk 001438826 85640 $$3Springer Nature$$uhttps://univsouthin.idm.oclc.org/login?url=https://link.springer.com/10.1007/978-3-030-79397-5$$zOnline Access$$91397441.1 001438826 909CO $$ooai:library.usi.edu:1438826$$pGLOBAL_SET 001438826 980__ $$aBIB 001438826 980__ $$aEBOOK 001438826 982__ $$aEbook 001438826 983__ $$aOnline 001438826 994__ $$a92$$bISE