Geoscience Reference
In-Depth Information
Cochonat et al.
2002
; Mazzotti et al.
2002
). It is characterized by multiple intraplate
shortenings and by recurrent earthquakes (Le Pichon et al.
1987
). The Tokai Thrust
(Fig.
1
) is one of the largest subhorizontal out-of-sequence thrusts within the
Nankai prism (Ashi et al.
2002
; Mazzotti et al.
2002
; Kawamura et al.
2009
). In
addition, the eastern Nankai prism is characterized by a steeper slope than the
Kumano region which is just on the study area (Cochonat et al.
2002
). In the eastern
Nankai prism, large-scale gravitational sliding is common, particularly between the
Kodaiba Fault and the Tokai Thrust (Cochonat et al.
2002
; Kawamura et al.
2009
,
2011 Chapter 10). The Tenryu Submarine Canyon cuts the geologic architecture
between the Kodaiba Fault and the Tokai Thrust (Figs.
1
and
2
). Therefore, the side
walls of the Tenryu Canyon show the vertical and lateral changes in intraprism
geologic architecture (Kawamura et al.
2009
, 2011 Chapter 10).
3
Occurrence of Samples and Dark Bands
The samples described in this study were collected by the 6K from three sites in the
Tenryu Canyon during cruises YK05-08 Leg 2 and YK08-E04 (Fig.
1
). Several
representative samples are described below.
3.1
6K#893 R-3
During cruise YK05-08 Leg 2, sample 6K#893 R-3 was collected from the Tokai
Thrust zone (Fig.
1
). This sample includes dark bands in two zones: DB-1 and
DB-2 (Fig.
3a
). The sample is composed of sandstone (SS), mudstone-1 (MS-1),
and mudstone-2 (MS-2; Fig.
3b
). DB-1 is a boundary between SS and MS-1, and
DB-2 is between MS-1 and MS-2. MS-1 and MS-2 have similar lithofacies and
include similar fine elongate grains and radiolarian fossils (Fig.
3b
). However, the
attitudes of the DB-1 and DB-2 bedding planes are different.
DB-1 is about 10 mm wide, whereas DB-2 is only a few mm wide. DB-1 and
DB-2 are parallel to the SS and MS-2 bedding planes, respectively. Both bands are
oblique to the bedding plane of MS-1 (Fig.
3a, b
). The upper and lower surfaces of
DB-2 are sharply defined and straight, whereas DB-1 has an undulating upper sur-
face. Because DB-2 cuts DB-1, DB-1 was formed before DB-2.
3.2
6K#1056 R6-2, 6K#1060 R2-1 and R2-2
During YK08-E04, three samples including dark bands were collected: 6K# 1056
R6-2 (Fig.
3c
), 6K#1060 R2-1 (Fig.
3e
), and 6K#1060 R2-2 (Fig.
3g
). Dive
6K#1056 was on the eastern wall of the Tenryu Canyon, south of the Tokai Thrust
and west of the Yukie Ridge (Kawamura et al.
2008
; Fig.
1
). There is a broad
Search WWH ::
Custom Search