Provenance of middle to late Miocene clastic sedimentary rocks in the central to eastern Cibao basin, northern Hispaniola /

and a southern source is the Cordillera Central.

Bibliographic Details
Main Author: Yao, Meng
Format: Thesis eBook
Language:English
Published: [Place of publication not identified] : [publisher not identified] ; 1997.
Subjects:
Online Access:Link to OAKTrust copy
Description
Summary:and a southern source is the Cordillera Central.
characteristics suggest that middle to late Miocene clastic
chlorite/illite ratio and varied feldspar abundance. Type 2
Cibao basin in northern Hispaniola has been assessed via
compositions determined by electron microprobe analysis
eastern Cibao basin display two geochemically distinctive
elements and rare earth elements (REE). Framework modes of
feldspar grains, and the distribution and abundance of trace
indicate derivation from plutonic, metamorphic, and possibly
integrated methods including detrital framework modes, clay
lower percentage of feldspar. These geochemical
mainly from recycled orogen provenance. Individual feldspar
margins setting. Multiple sources are suggested by this
middle to late Miocene clastic samples suggest a source
mineral assemblages and ratios, the composition of individual
REE, Th, Sc and Cr+Ni values, correspond to relatively higher
sediments in Cibao basin are related to an active continental
sediments, with relatively higher total REE, Th, Sc and Cr+Ni
study. A northern source is the Cordillera Septentrional,
that the middle and late Miocene sediments in the central to
The provenance of middle to late Miocene clastic sediments of
type features. Type 1 sediments, with relatively lower total
values, are consistent with lower chlorite/illite ratio and
volcanic sources. Trace elements and REE data demonstrate
Item Description:"Major subject: Geology".
Vita.
Physical Description:xi, 110 leaves : illustrations, maps ; 28 cm.
Also available online.
Issued also on microfiche from Lange Micrographics.
Bibliography:Includes bibliographical references.