The Middle America Trench in the geological framework of Central America ( DSDP, Leg 67).

10Citations
Citations of this article
14Readers
Mendeley users who have this article in their library.

Abstract

The tectonic framework of the Middle America Trench is composite. In its N part, the Trench runs along the North American continent (at the least, along Mexico up to the Guatemala Transverse Zone; at the most, up to the Honduras Platform). In this part the Trench is not related to the tectonic features of Mexico, which it cuts very obliquely, and is thus a recent neotectonic feature. In its S part, the Isthmus of Central America is a tectonic edifice (with a strike like that of the Trench) supporting a huge Tertiary volcanic cover; in this part, the Trench could have originated from an ancient subduction zone involving Mesozoic oceanic sediments and crust. Along the Guatemala Transverse Zone the following events took place: at the end of the Cretaceous, a big overthrust of Central American-Caribbean ophiolitic facies occurred towards the N, at the termination of the North American continent; and during the Pliocene to Quaternary.-from Authors

Cite

CITATION STYLE

APA

Aubouin, J. (1982). The Middle America Trench in the geological framework of Central America ( DSDP, Leg 67). Initial Reports DSDP, Leg 67, Manzanillo to Puntarenas, Costa Rica, 747–755.

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free