New Articles for Geosphere Posted Online in August
Boulder, Colo., USA: GSA’s dynamic online journal, Geosphere,
posts articles online regularly. Locations and topics studied this month
include Death Valley, the San Andreas fault; and Haleakala volcano’s crater
and great valleys. You can find these articles at
https://geosphere.geoscienceworld.org/content/early/recent
.
Landslide hypothesis for the origin of Haleakala volcano’s crater and
great valleys, Hawaii
Kim M. Bishop
Abstract:
Active Haleakala volcano on the island of Maui is the second largest
volcano in the Hawaiian Island chain. Prominently incised in Haleakala's
slopes are four large (great) valleys. Haleakala Crater, a prominent summit
depression, formed by coalescence of two of the great valleys. The great
valleys and summit crater have long been attributed solely to fluvial
erosion, but two significant enigmas exist in the theory. First, the great
valleys of upper Keanae/Koolau Gap, Haleakala Crater, and Kaupo Gap are
located in areas of relatively low annual rainfall. Second, the axes of
some valley segments are oblique for long distances across the volcanic
slopes. This study tested the prevailing erosional theory by reconstructing
the volcano's topography just prior to valley incision. The reconstruction
produces a belt along the volcano's east rift zone with a morphology that
is inconsistent with volcanic aggradation alone, but it is readily
explained if it is assumed the surface was displaced along scarps formed by
a giant landslide on Haleakala's northeastern flank. Although the landslide
head location is well defined, topographic evidence is lacking for the toe
and lateral margins. Consequently, the slope failure is interpreted as a
sackung-style landslide with a zone of deep-seated distributed shear and
broad surface warping downslope of the failure head. Maximum downslope
displacement was likely in the range of 400–800 m. Capture of runoff at the
headscarps formed atypically large streams that carved Haleakala's great
valleys and explains their existence in low-rainfall areas and their
slope-oblique orientations. Sackung-style landslides may be more prevalent
on Hawaiian volcanoes than previously recognized.
View article:
https://pubs.geoscienceworld.org/gsa/geosphere/article-abstract/doi/10.1130/GES02215.1/607272/Landslide-hypothesis-for-the-origin-of-Haleakala
Detrital zircon provenance and depositional links of Mesozoic Sierra
Nevada intra-arc strata
Snir Attia; Scott R. Paterson; Jason Saleeby; Wenrong Cao
Abstract:
A compilation of new and published detrital zircon U-Pb age data from
Permo-Triassic to Cretaceous intra-arc strata of the Sierra Nevada (eastern
California, USA) reveals consistent sedimentary provenance and depositional
trends across the entire Sierra Nevada arc. Detrital zircon age
distributions of Sierra Nevada intra-arc strata are dominated by Mesozoic
age peaks corresponding to coeval or just preceding arc activity. Many
samples display a spread of pre-300 Ma ages that is indistinguishable from
the detrital age distributions of pre-Mesozoic prebatholithic framework
strata and southwestern Laurentian continental margin deposits. Synthesis
of detrital zircon age data with tectonostratigraphic constraints indicates
that a marine to subaerial arc was established in Triassic time, giving way
to widespread shallow- to deep-marine deposition in latest Triassic to
Early Jurassic time that continued until the emergence of the arc surface
in the Early Cretaceous. No data presented herein require the existence of
Mesozoic exotic terranes and/or outboard arcs that were previously
hypothesized to have been accreted to the Sierra Nevada. We conclude that
Sierra Nevada intra-arc strata formed within a coherent depositional
network that was intimately linked to the southwestern United States
Cordilleran margin throughout the span of Mesozoic arc activity.
View article:
https://pubs.geoscienceworld.org/gsa/geosphere/article-abstract/doi/10.1130/GES02296.1/607274/Detrital-zircon-provenance-and-depositional-links
Superposition of two kinematically distinct extensional phases in
southern Death Valley: Implications for extensional tectonics
Z.D. Fleming; T.L. Pavlis; S. Canalda
Abstract:
Geologic mapping in southern Death Valley, California, demonstrates
Mesozoic contractional structures overprinted by two phases of Neogene
extension and contemporaneous strike-slip deformation. The Mesozoic folding
is most evident in the middle unit of the Noonday Formation, and these
folds are cut by a complex array of Neogene faults. The oldest identified
Neogene faults primarily displace Neoproterozoic units as young as the
Johnnie Formation. However, in the northernmost portion of the map area,
they displace rocks as young as the Stirling Quartzite. Such faults are
seen in the northern Ibex Hills and consist of currently low- to
moderate-angle, E-NE– dipping normal faults, which are folded about a
SW-NE–trending axis. We interpret these low-angle faults as the product of
an early, NE-SW extension related to kinematically similar deformation
recognized to the south of the study area. The folding of the faults
postdates at least some of the extension, indicating a component of
syn-extensional shortening that is probably strike-slip related.
Approximately EW-striking sinistral faults are mapped in the northern
Saddlepeak Hills. However, these faults are kinematically incompatible with
the folding of the low-angle faults, suggesting that folding is related to
the younger, NW-SE extension seen in the Death Valley region. Other faults
in the map area include NW- and NE-striking, high-angle normal faults that
crosscut the currently low-angle faults. Also, a major N-S–striking,
oblique-slip fault bounds the eastern flank of the Ibex Hills with
slickenlines showing rakes of <30°, which together with the map pattern,
suggests dextral-oblique movement along the east front of the range. The
exact timing of the normal faulting in the map area is hampered by the lack
of geochronology in the region. However, based on the map relationships, we
find that the older extensional phase predates an angular unconformity
between a volcanic and/or sedimentary succession assumed to be 12–14 Ma
based on correlations to dated rocks in the Owlshead Mountains and
overlying rock-avalanche deposits with associated sedimentary rocks that we
correlate to deposits in the Amargosa Chaos to the north, dated at 11–10
Ma. The mechanism behind the folding of the northern Ibex Hills, including
the low- angle faults, is not entirely clear. However, transcurrent systems
have been proposed to explain extension-parallel folding in many
extensional terranes, and the geometry of the Ibex Hills is consistent with
these models. Collectively, the field data support an old hypothesis by
Troxel et al. (1992) that an early period of SW-NE extension is prominent
in the southern Death Valley region. The younger NW-SE extension has been
well documented just to the north in the Black Mountains, but the potential
role of this earlier extension is unknown given the complexity of the
younger deformation. In any case, the recognition of earlier SW-NE
extension in the up-dip position of the Black Mountains detachment system
indicates important questions remain on how that system should be
reconstructed. Collectively, our observations provide insight into the
stratigraphy of the Ibex Pass basin and its relationship to the extensional
history of the region. It also highlights the role of transcurrent
deformation in an area that has transitioned from extension to
transtension.
View article:
https://pubs.geoscienceworld.org/gsa/geosphere/article-abstract/doi/10.1130/GES02354.1/607022/Superposition-of-two-kinematically-distinct
Latest Quaternary slip rates of the San Bernardino strand of the San
Andreas fault, southern California, from Cajon Creek to Badger Canyon
Sally F. McGill; Lewis A. Owen; Ray J. Weldon; Katherine J. Kendrick; Reed
J. Burgette
Abstract:
Four new latest Pleistocene slip rates from two sites along the
northwestern half of the San Bernardino strand of the San Andreas fault
suggest the slip rate decreases southeastward as slip transfers from the
Mojave section of the San Andreas fault onto the northern San Jacinto fault
zone. At Badger Canyon, offsets coupled with radiocarbon and optically
stimulated luminescence (OSL) ages provide three independent slip rates
(with 95% confidence intervals): (1) the apex of the oldest dated alluvial
fan (ca. 30–28 ka) is right-laterally offset ~300–400 m yielding a slip
rate of 13.5 +2.2/−2.5 mm/yr; (2) a terrace riser
incised into the northwestern side of this alluvial fan is offset ~280–290
m and was abandoned ca. 23 ka, yielding a slip rate of 11.9 +0.9
/−1.2 mm/yr; and (3) a younger alluvial fan (13–15 ka) has been
offset 120–200 m from the same source canyon, yielding a slip rate of 11.8 +4.2/−3.5 mm/yr. These rates are all consistent and
result in a preferred, time-averaged rate for the past ~28 k.y. of 12.8 +5.3/−4.7 mm/yr (95% confidence interval), with an
84% confidence interval of 10–16 mm/yr. At Matthews Ranch, in Pitman
Canyon, ~13 km northwest of Badger Canyon, a landslide offset ~650 m with a 10Be age of ca. 47 ka yields a slip rate of 14.5 +9.9
/−6.2 mm/yr (95% confidence interval). All of these slip rates
for the San Bernardino strand are significantly slower than a previously
published rate of 24.5 ± 3.5 mm/yr at the southern end of the Mojave
section of the San Andreas fault (Weldon and Sieh, 1985), suggesting that
~12 mm/yr of slip transfers from the Mojave section of the San Andreas
fault to the northern San Jacinto fault zone (and other faults) between
Lone Pine Canyon and Badger Canyon, with most (if not all) of this slip
transfer happening near Cajon Creek. This has been a consistent behavior of
the fault for at least the past ~47 k.y.
View article:
https://pubs.geoscienceworld.org/gsa/geosphere/article-abstract/doi/10.1130/GES02231.1/607021/Latest-Quaternary-slip-rates-of-the-San-Bernardino
Geological and seismic evidence for the tectonic volution of the NE
Oman continental margin and Gulf of Oman
Bruce Levell; Michael Searle; Adrian White; Lauren Kedar; Henk Droste ...
Abstract:
Late Cretaceous obduction of the Semail ophiolite and underlying thrust
sheets of Neo-Tethyan oceanic sediments onto the submerged continental
margin of Oman involved thin-skinned SW-vergent thrusting above a thick
Guadalupian–Cenomanian shelf-carbonate sequence. A flexural foreland basin
(Muti and Aruma Basin) developed due to the thrust loading. Newly available
seismic reflection data, tied to wells in the Gulf of Oman, suggest
indirectly that the trailing edge of the Semail Ophiolite is not rooted in
the Gulf of Oman crust but is truncated by an ENE-dipping extensional fault
parallel to the coastline. This fault is inferred to separate the Semail
ophiolite to the SW from in situ oceanic Gulf of Oman crust to the NE. It
forms the basin margin to a “hinterland” basin formed atop the Gulf of Oman
crust, in which 5 km of Late Cretaceous deep-water mudstones accumulated
together with 4 km of Miocene and younger deep-water mudstones and
sandstones. Syndepositional folding included Paleocene–Eocene folds on N-S
axes, and Paleocene to Oligocene growth faults with roll-over anticlines,
along the basin flank. Pliocene compression formed, or tightened, box folds
whose axes parallel the modern coast with local south-vergent thrusts and
reversal of the growth faults. This Pliocene compression resulted in
large-scale buckling of the Cenozoic section, truncated above by an
intra-Pliocene unconformity. A spectacular 60-km-long, Eocene(?) to Recent,
low-angle, extensional, gravitational fault, down-throws the upper basin
fill to the north. The inferred basement of the hinterland basin is in situ
Late Cretaceous oceanic lithosphere that is subducting northwards beneath
the Makran accretionary prism.
View article:
https://pubs.geoscienceworld.org/gsa/geosphere/article-abstract/doi/10.1130/GES02376.1/607023/Geological-and-seismic-evidence-for-the-tectonic
Geometrical Breakdown Approach to interpretation of depositional
sequences
Masoud Aali; Bill Richards; Mladen R. Nedimović; Vittorio Maselli; Martin
R. Gibling
Abstract:
Seismic and sequence stratigraphic analyses are important methodologies for
interpreting coastal and shallow-marine deposits. Though both methods are
based on objective criteria, terminology for reflection/stratal stacking is
widely linked to eustatic cycles, which does not adequately incorporate
factors such as differential subsidence, sediment supply, and autogenic
effects. To reduce reliance on model-driven interpretations, we developed a
Geometrical Breakdown Approach (GBA) that facilitates interpretation of
horizon-bound reflection packages by systematically identifying
upward-downward and landward-seaward trajectories of clinoform inflection
points and stratal terminations, respectively. This approach enables a
rigorous characterization of stratal surfaces and depositional units. The
results are captured in three-letter acronyms that provide an efficient way
of recognizing repetitive stacking patterns through discriminating
reflection packages objectively to the maximum level of resolution provided
by the data. Comparison of GBA with selected sequence stratigraphic models
that include three and four systems tracts and the accommodation succession
approach shows that the GBA allows a greater level of detail to be
extracted, identifying key surfaces with more precision and utilizing more
effectively the fine-scale resolution provided by the input seismic data.
We tested this approach using a synthetic analogue model and field data
from the New Jersey margin. The results demonstrate that the geometric
criteria constitute a reliable tool for identifying systems tracts and
provide an objective and straightforward method for practitioners at all
levels of experience.
View article:
https://pubs.geoscienceworld.org/gsa/geosphere/article-abstract/doi/10.1130/GES02371.1/607024/Geometrical-Breakdown-Approach-to-interpretation
GEOSPHERE articles are available at
https://geosphere.geoscienceworld.org/content/early/recent
. Representatives of the media may obtain complimentary copies of GEOSPHERE
articles by contacting Kea Giles at the address above. Please discuss
articles of interest with the authors before publishing stories on their
work, and please refer to GEOSPHERE in articles published. Non-media
requests for articles may be directed to GSA Sales and Service, gsaservice@geosociety.org.
https://www.geosociety.org/
# # #