T223 Structural Analysis, Digital Mapping Advances, Tectonics, and Tectonic-Climate Processes from California to Alaska and Elsewhere II: A Celebration of Terry Pavlis’s Diverse Contributions and Career

Tuesday, 24 September 2024
1:30 PM - 5:30 PM
304A


TERRANE TECTONICS: WHERE HAVE WE COME FROM AND WHERE ARE WE GOING?

Paper number: T223-6
Program: Technical Sessions
Time: 2:50 PM – 3:05 PM


Authors


Abstract

The development of the terrane concept and tectonic syntheses derived from it was arguably a major advance in the understanding of Cordilleran tectonics, yet the methods carried intellectual baggage that have led to seemingly unresolvable paradoxes. In this presentation we review original concepts presented in terrane analysis, note pros and cons of the method, and present examples of where the methods shone and greatly advanced our understanding of a region’s history, and examples of where the method failed. We also consider examples of cases where a “house of cards” developed, in which tectonic models are based on accumulations of interpretations such that the interpretations became akin to observations. One example of misuse of terrane nomenclature results in excessive “splitting”, a particular problem in major fault zones and subduction complexes; taken to an extreme, every block in a mélange could be a picoterrane. The other type of extreme produced by some terrane terminology occurs when overzealous correlations lump assemblages with limited primary stratigraphic continuity via inferred correlations across complexly deformed zones. The latter is a particularly significant divergence from the original concept of “suspect terranes” where the burden of proof of correlation was a hard rule. We contend many of these problems are resolvable if researchers return to key areas, freed from blinders imposed by previous syntheses, and deploy a full suite of modern methods focused on resolving key issues.

Geological Society of America Abstracts with Programs. Vol. 56, No. 5

doi: 10.1130/abs/2024AM-401727

© Copyright 2024 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.